All items from The Why Files

Aches and pains? Blame the ancestors

It’s the middle of February, and the world is learning that Oscar Pistorius, a sprinter who ran in the Olympics, has been charged with murdering his girlfriend. In the summer of 2012, Pistorius, the first double amputee Olympic athlete, a hero for his personal grit.

His ultra-efficient carbon feet, inevitably, led to the nickname “blade runner.”

The carbon blades that enabled Oscar Pistorius to race in the 2012 Olympics are strong, springy and fast. Rollover to see the structure of your foot. “This prosthetic looks almost nothing like a human foot,” says Jeremy DeSilva of Boston University. “It has a single rigid element, strong enough to push off the ground, elastic enough to put a kick into the step.”
Photos: Will Clayton (Pistorius), Ryan Lines (x-ray)

At the annual meeting of the American Association for the Advancement of Science, the news about blade runner served as an ideal but sad lead-in for Jeremy DeSilva, an anthropologist at Boston University who studies body structure. Comparing photos of the blades to an X-ray of the foot, DeSilva observed drily that “The [human] foot is not what you would design from scratch.”

Instead of this single bladelike structure, he said, “our foot has 26 bones. Our ape relatives have 26, and that’s the story in the primate line. Many problems we have today are the result of that.”

Our tree-climbing primate ancestors needed a foot able, like their hands, to grab and hold. Now that we are walking on our feet, those moving parts lead to sprained ankles, heel spurs, collapsed arches, Achilles tendinitis, osteoarthritis and plantar fasciitis, says DeSilva. “It all goes back to upright walking.”

Evolution ≠ perfection

Evolution is the organizing principle of biology: a fact of life. Plants and animals that look alike usually share common ancestors. Organisms that have similar genes got them from the same ancestor. And ditto for creatures with similar proteins.

Evolution is driven by selection: The genes of organisms that can survive and produce offspring are represented in the next generation. Genes that fail these twin tests disappear.

But just because evolution has crafted millions of working answers to survival and reproduction does not make the results ideal. “It’s been known for a long time, since Darwin, that evolution does not produce perfection,” says DeSilva. “Evolution works from raw material that was previously created, and it modifies and tinkers with it, producing the biological equivalent of duct tape and paperclips. If the organism survives, passes along its genes, then off we go.”

The genes and structures — like the spine, digestive tract or brain — most conducive to survival and reproduction are repeated, often with modification due to chance mutation.

Instead of inventing from whole cloth, evolution works through a “good-enough” process called descent with modification.

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Two-toed leathery claws of an ostrich as it stands on dirt.

Photo: kibuyu
This young ostrich, from Kenya, shows off a foot that can sprint and deliver a swift kick in the rear, using surprisingly few moving parts.

And that brings us to the “scars of evolution,” a theory proposed in 1951 by Wilton Krogman that proposes to explain a number of human shortcomings. DeSilva was one of several scientists at the February meeting who blamed our woes on the ones who came before — the predecessor primates and other mammals whose genes still largely control our fate.

Got the walking blues

Human foot problems are sometimes blamed on shoes, sidewalks, or the life of a couch potato, but DeSilva says nay. “It’s amazing how the fossil record indicates that foot problems go back into the past.”

Some feet have much better design. The ostrich for example, is a biological version of the sprinter’s carbon blades. “Ostriches have a fused bone at the ankle,” DeSilva says, “and big tendons that give it that elastic energy, that kick.”

Blame the ancestors. Birds, DeSilva says, “had a 230-million year head start on us, because they evolved from bipedal dinosaurs,” while people have only been walking on two feet for 4 or 5 million years. “Our ancestors were quadrapedal, spending a good deal of time in the trees, and they evolved this very mobile, grasping foot, made for living in the trees.”

When great-grandma started walking upright, evolution began to remodel her foot, stabilizing it with oodles of ligaments, “But these were Band-Aids,” DeSilva says. “Natural selection did wonders to modify the ape foot so we could walk on two legs, but that led to problems.”

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Model of human foot showing bones and ligaments.

Those ligaments, shown in blue, attempt to stabilize a foot built for climbing trees so it can stroll the boulevard and run a marathon.

The in-and-out rotation of the ankle helped our ancestors grab limbs, but it also facilitates sprains. And if you stand on one leg, DeSilva says, “You wobble; the ankle is very unstable, and you do this every single time you take a step.”

Through the process of convergent evolution (similar structures arising from different predecessors) foot bones have fused in some mammals that have been walking for millions of years. “In the horse and the antelope, the ankle is reduced in size, the metatarsal bones have fused, and the pedal digits have reduced to one,” says DeSilva. “That’s biomechanically better.”

No sense searching for a collapsed arch in an ostrich or a horse (both sprinters that could outrun blade runner). “You can’t get a collapsed arch if you don’t have an arch,” DeSilva says.

Understanding the evolution of the structure that helps us stand, walk and run shows that evolution is not just “a dusty old science, behind glass in a museum,” says DeSilva. “Our evolutionary history explains why we are the way we are today. Evolution impacts us today.”

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Cat skeleton with all four paws on ground, in walking position.

Photo: Cliff
This Australian native cat, Dasyurops maculatus, shows one major arch in the back.
Engraving of human skeleton upright, in walking position.
This skeleton shows the three major curves of our spine (from top): cervical, thoracic and lumbar.
Modified from original engraving “Die Gesammten Naturwissenschaften für das Verständnis weiterer Kreise,” published in Essen, Germany, Georg Holderied

Backed into a corner

Worldwide, back problems are humanity’s number-six ailment, says Bruce Latimer, professor of anthropology at Case Western Reserve University. Among musculoskeletal issues, backs rank first. “If you want a place that is really a problem, it’s the back,” he says cheerfully.

Back trouble is rooted in our descent from animals who walked on all fours, with the back in a horizontal position. The transition to the vertical entailed an extra curve to balance the weight over the hips, and while these curves alleviate the shock of walking, they are “a recipe for trouble,” Latimer says.

The spine is built of vertebrae and disks, and “If I gave you 24 cups and saucers, each representing a vertebra or a disk, if you were really careful, you could stack them,” Latimer says. “Now I want you to add in those curves, and if I gave you all the duct tape in the world, you could not possibly do it.”

The pronounced lumbar curve is found in no other mammal, Latimer says. Add in that reverse curve in the thorax, and a third in the neck, “and you wonder why there is a problem?”

On the plus side, our spine is highly flexible, and we are the only mammal that can do a back bend. Twisting and bending have other benefits, Latimer says. “Apes get disk infections because they don’t have a flexible spine, so they have trouble pumping nutrients into their disks.”

Disking disaster

Those disks, however, can get crunched by gravity and stresses due to our upright gait, Latimer says. “As we walk, we throw our upper body 180° out of synch with the lower body, as the right arm goes forward, so does the opposite leg. We are constantly twisting, torqueing the spine, and ultimately after millions of repetitions, we wear through the fibrous exterior of the disk.”

Twisting and compression can translate into a disk that is “slipped” or “herniated,” as the soft center bulges and compresses the nerves, creating excruciating back and leg pain known to millions. “If you live long enough, you will have a herniated disk,” says Latimer.

Evolution tried to compensate with larger vertebrae, which reduce bulging and popping in the disks, but these big vertebra are built of porous — and therefore weaker — bone. “When we have the endocrine shift at menopause, women lose bone, and get osteoporosis,” says Latimer.

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Model of vertebra and disks, showing bulging herniated disk.

Modified from original image by Michael Dorausch
Disks separate the vertebra, but pain can result when they deform and compress the nerves.

The great apes do not lose bone mass as they age, but neither do they get the spine-bending disability scoliosis.

After Charles Darwin first published his theory of evolution in 1859, scientists looked to it for explanations of the structures visible in plants and animals. Now, they realize that evolution has present-day significance. “Evolution tinkers with what it has, can’t create perfection; it can’t invent a brand new spine,” says Latimer. “If you think [the spine] is an intelligently designed structure, I suggest you get a new engineer.”

Teeth: Scars being solved!

Describing what he called the “final drop in the bucket of how you are going to fall apart,” Alan Mann, professor of anthropology at Princeton University, focused on the “wisdom tooth,” or third molar, which often jams instead of emerging in young adulthood.

This is supposedly the time when teenagers get “wisdom,” but instead a pain gnaws their jaw!

Teeth are the opening gambit of the digestive system. The front teeth are shaped to tear away food and the back teeth shaped for grinding and shearing food before swallowing and digestion.

The emergence of human teeth is tightly choreographed: The baby teeth start appearing at roughly age one, and later are replaced by the adult teeth as the mouth enlarges. The tough diets of our ancestors quickly wore the teeth, so it made sense for a brand-new molar — the third — to emerge after puberty.

That midget brain fitted quite nicely above the triplet of molars in this portrayal of Sahelanthropus tchadensis, a human ancestor from about 7 million years ago. Rollover to see a modern head, where the brain has moved up and forward, leaving less space for three molars.
Credit: dctim1 and illuminaut

But once the human brain expanded, the brain moved from behind the face to above it, leaving less room for the teeth, and the result, often, was an impacted wisdom tooth.

And the big brain (it’s three times as big as our ancestors’) Mann says, is the ultimate reason why wisdom teeth get stuck.

That’s the evolutionary bad news. The good news is that a random mutation thousands of years ago that prevents the third molar from hardening is spreading as evolution selects against wisdom teeth. Among some populations, 40 percent of people lack at least one third molar.

Impacted wisdom teeth are seldom fatal, so why would they shape our evolution? To answer, Mann offers this scenario: “One evening, a person who had chronic pain from an impacted tooth is asked, ‘How about a bout of reproduction, dear?” and responds, ‘Not tonight, my jaw is killing me.’” The result, he says, could be fewer offspring for the unlucky adults with impacted third molars.

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Xray of three normally-positioned human molars and a fourth turned on its side, growing into the others.

This lower wisdom tooth is impacted — useless at best and likely to be painful or even infected. But evolution to seems be eliminating this affliction of young adulthood.

So evolution is not just a source of scars, but also of solace, Mann says. “In the course of human evolution, as the amount of space [in the jaw] became smaller, a random mutation had selective value, and its frequency increased over time. But the third molar remains a scar of human evolution when dental technology [surgery] is not available.”

Birth: the most perilous escape

“If you want an example of something that is not intelligently designed, think about the crazy, tricky, complicated, uncomfortable way we have babies,” says Karen Rosenberg, chair of anthropology at the University of Delaware. “Childbirth is a time in the life cycle where women and babies are under increased risk of injury or death.”

These difficulties “go way back in evolutionary history, possibly back to the beginning of bipedalism,” she says. Our ancestors, after all, lived in trees and were much better at climbing than walking, which they did on all fours.

Efficient upright walking requires narrow hips, which shrinks the birth canal in the pelvis. But the birth canal must still accommodate that pesky-big human head.

Several evolutionary adaptations permit this awkward birth, Rosenberg says:

While apes are born with a fused skull, ours remain flexible until after birth. (The ability to change shape during birth explains the “cone-head” seen after a difficult vaginal birth)

Human infants are born earlier in development than other primates, so our brain is further from full size

Our head rotates during birth to fit the birth canal

Our mothers and infants get support during birth (and for years afterward)

Culture is critical during birth, Rosenberg says. After the head rotates, “the baby usually turns and emerges facing back. And so there is a benefit to having someone there to catch the baby.”

A group of women sit in a classroom with anatomical models in the background.
Photo: UNAMID
Young women learn how pregnancy affects the pelvis at the School for Midwifes in Elfasher, Sudan, as they prepare to assist in childbirth.

Attended birth is essentially unknown among our relatives, Rosenberg says. “Other primates give birth without assistance, in isolation. Humans give birth socially, and midwives around the world know all kinds of different things that ameliorate the risk. We are able to mitigate the risks because we are cultural animals; we have someone there to help when in labor.”

The result is a positive feedback among brain size, intelligence and culture, Rosenberg says. “The fact that we give birth in such a risky way speaks to the benefit accrued by having such a large brain. We are able to have culture because we have a large brain, and are able to have a large brain because we ameliorate the risks of childbirth culturally.” Even though childbirth remains hazardous, “This tells us how beneficial it is to have large brain, and the complex behavior we have as humans.”

The benefits of culture continue past birth, Rosenberg says. “It’s because we are cultural animals that we can take care of a baby that is born earlier, wrap it in a blanket, use a cradle board to prevent injury to the neck.”

All story long, we have been hearing complaints about the jury-rigged equipment we inherited from our ancestors — feet with too many bones, unstable spines, and teeth that get stuck instead of emerging on schedule. But “childbirth is not a scar of evolution,” Rosenberg insists. “The evolution of a rotating head during birth allowed this continual increase in brain size; we came to a point where the brain could not get bigger” unless we had culture to support the mother and infant. “Childbirth is an ancient and fundamental part of what makes us human.”

– David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Dear Whyfiles

Dear Why Files:

I don’t get it. I’m a plain ol’ mole, and my self-image is in the toilet. Sure, I dig a lot of holes as I chase insects and earthworms. People blame me for wrecking their silly lawns, but that’s nothing compared to a squirrel in the attic or a Canada goose laying “cigars” on the grass. And I’m no rabid dog: I don’t make people sick. And I can’t remember the last time anybody asked to take my photo! Even though we live underfoot, we still have feelings!

–Depressed Digger

Dear Depressed Digger

I sympathize. Sure, moles are short on charisma, and that all-subterranean-all-the-time lifestyle is a real recipe for cabin fever.

But you’re making a mountain from a molehill! I’ve just heard from an admirer in Tennessee who thinks you can do what nobody else can: smell in stereo! Fifty-plus years after record companies began selling discs that deliver a different sound to each speaker, and 500 million years (just wild-guessing now) after animals began using two eyes to get a better picture of their environs, Kenneth Catania, a professor of biology at Vanderbilt University, says you may be the only animal proven to smell in stereo.

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Large claws of mole splay grass as it pokes out of hole in ground

Wikipedia
The eastern mole (Scalopus aquaticus) lives entirely underground, devouring earthworms that it detects with a super schnozzola.

You, the innocent and invisible common mole, AKA the eastern mole. Feeling better already?

Separate, but equal?

The idea that the sensory nerves behind each nostril may deliver different information to the brain “has been out there, people have been curious for a long time,” Catania says. “Paired eyes and ears are important for stereo vision, depth perception, and sound localization, so it’s natural to wonder” if having two nostrils would help locate the source of an odor.

But Catania says he started out “a big skeptic. I thought the nostrils [in the common mole] were so close together, what are the chances they could localize a smell?”

Catania says he’d been looking at the starnose mole “which has an incredible sense of touch” (though evolution has given it a rather strange mug). He said you, the common mole, “have the worst sense of touch among the mole species,” so he was sure you would be a fumbling idiot when you had to search for food.

Instead, Catania says, you “went straight toward the food. I am not sure there is any study in mammals that shows a better localization of an odorant” in a test chamber.

Everybody gets to be a champion!

Furry mole head with several pink tendrils extending from nose pokes out of hole in ground
The star-nose mole uses its exquisite sense of touch to find food.

Catania was smart enough to wonder if common moles could be smelling in stereo. “It was very hard to explain how they doing so well otherwise,” he says. Knowing that you “would do anything if is there is an earthworm at the end of it,” he put you into a test chamber with a bit of earthworm as bait, and counted how long it took you to find it.


Courtesy Kenneth Catania, Vanderbilt University
Double-click on movie to watch a double-speed image of a common mole finding bait in the test chamber; followed by a mole with one nostril blocked.

Immediately, you started wriggling your nose and moving around, kinda like people try to locate a “present” from their dog.

And in as little as five seconds of frantic sniffing, you found the bait.

Then the fun began. When Catania plugged your right nostril, you following the stronger scent on the right, veered too far left, but eventually homed in on your reward. But when he hooked your sniffer up to a crisscross pipe, so each nostril smelled the opposite side, you were bewildered and never found the bait.

The discovery of stereo smelling is sexy, but Catania notices that you start out using the more common sniff-move-sniff technique, and then switch to stereo-smelling when you got closer to the pay dirt.

No offense, but we asked Catania why this mattered. He admitted that “a lot of it is just inherently cool. But I’m always amazed at what animals can do. I will be studying them for one reason, and they tell me something completely different. When I went into this, I thought the common mole would have poor foraging ability due to its poor sense of touch, but they were off-the-scale good in another way.”

So chin up, Depressed Digger: As far as your self-image is concerned, there’s light at the end of the tunnel! Not that you can actually see it, unfortunately…

— David J. (Not Ann Landers) Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Huge white and orange-tinted clouds against blue sky above green landscape.

Typically, the swirl of stormy weather obscures the cells at the heart of severe thunderstorms. This uncommonly clear view of an entire thunderstorm cell, with the top of the growing cumulonimbus tower topping out at 40,000 feet, reveals many interesting features, including “fall streaks” of what may be hail from the underside of the overhanging anvil portion of the cloud. Shortly after this photo was taken on May 22, 2011, near Madison, the storm pelted the Sun Prairie area with large, damaging hail. Courtesy Grant W. Petty, Cool Science Image 2012 Contest Winner

Flowers: More seductive than ever

Many plants need insects to import pollen to fertilize their eggs and start making seeds. To attract these pollinators, flowers advertise with scents, colors and patterns.

Bee covered in yellow dust, pollen, crouches atop small yellow flower.
This honeybee has slathered herself in pollen; some goes back to the hive, and some pollenates the flowers she is visiting.

And now we hear that some plants also use electric billboards to lure their six-legged colleagues.

The plants don’t act deliberately, but their electric field nonetheless communicates with bees, says Daniel Robert, a specialist in insect sensation at the University of Bristol, in the United Kingdom.

Robert, the corresponding author of a study in tomorrow’s Science magazine, says he was intrigued that bees acquire a positive charge during flight, which holds negatively-charged pollen through electrostatic attraction. “A pollen grain needs to stick to the bee, but not too much, so it can be deposited on the next flower,” Robert says. “I thought maybe this electric field was more important than just attraction.”

Pollination is a matter of life and death for many flower species: if insects don’t truck in the pollen, the essential cross-pollination fails, and the plant makes no seeds.

Thus evolution has shaped the flower to be “an extremely manipulative organ when it comes to attracting the bee,” says Robert. Pollen is a protein-rich bee food, and nectar is a sugary delight.

Sending bumblebees to bee school

You maybe didn’t know that bumblebees are trainable. Likewise. But in a series of experiments, Robert found that bumblebees learn to associate the electric field from a fake flower with the presence of sugar.

In soil: Jem Hologram, bee: Lisa Lawley
Bumblebees live the soil, in colonies of a few dozen members. Rollover to see a portrait of the bumblebee.

Visually, the fake flowers were identical, but some emitted no electric field, others had a 10-volt or 30-volt field. Some of the flowers carried a sweet reward — sucrose — while the others delivered super-bitter quinine. “Bees do not like the taste of quinine, and they learned to go to the sucrose, but it took 40 to 50 visits to reach an 80 percent correct rate,” says Robert.
Plants are rooted in the Earth and thus have a neutral or slightly negative charge, while bees accumulate a positive charge as they fly, creating an electric field between plants and bees.
Without the 30-volt cue, the bees could not find the sucrose, “so the information from the electric field was vital.” A 30-volt field is roughly what exists in a flower 30 centimeters tall.

Flower emitting 30 volts quickens bee’s flower-finding by ~25% over flowers with low or no field.
Adapted from Clarke et al. 2013
Fake flowers did not alter bee behavior if they emitted no voltage or 10 volts, but a 30-volt field around the flower led to 80 percent accuracy after 40 bee visits. The stronger field taught the bees which flowers had sugar, and which had bitter quinine.

“It was known before that bees would charge up as they fly through the atmosphere, and that flowers have a negative electric potential compared to the atmosphere, but we are the first to show that bees can detect the field, and can learn to discriminate between different fields,” Robert says.

Water is a great conductor of electric fields, and sharks, skates and other fish use electricity for sensory purposes. “But in terrestrial creatures, this process of recognizing electric fields is unique as far as we know, says Robert.

It’s possible that many insects use electric fields, Robert says. “There is no reason to think that any flying insect that goes through the air will not have this electric potential, because it is physically inevitable that you will accumulate a charge when flying through an ionic medium.”

The economy of flowers

The flowers seem to be an innocent bystander, not taking active charge of their charge, but why did bees evolve a receptor for electric fields, and the neural circuitry necessary to use the sensory input to change their behavior?

The answer resides in evolutionary economics, says Robert. “If a flower attracts too many bees, the nectar that they feed on will run out,” and that could spell disaster for both sides.

“If the flowers start to lie to the bees,” Robert says, “that’s not too good, as the bees are quick to learn which flowers are not good, and then they go back to the hive and say, ‘Let’s go to another place.’”

Two fuchsia horn-shaped flowers ringed with white on petal border.
Photo: Scott Zona
If color, scent and pattern are all signals to pollinators, we don’t know how insects will respond to this beautiful petunia!

And bees can’t waste too much time visiting dry flowers.

Open for business!

But neither flower color nor scent registers the state of the nectar supply, Robert says. So how can flowers tell the bees they need some slack time to produce more nectar?

With the electric field, which gets weaker when a bee lands to gather pollen, and even more when a second bee arrives.

To the bee’s still mysterious electrical detector, Robert says, “some of the flowers look bright, and some are dim, which means they have been visited a few minutes before. And when they are out foraging, this means the bees can avoid a negative reward. It means the advertisement is honest, and it’s changing from minute to minute.”

We learn to rely on ads that accurately reflect conditions, Robert adds. “When you drive in your car, and the motel sign says ‘Vacancy,’ you might stop. When it say ‘No Vacancy, you don’t. You have learned to trust the sign.”

— David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Bibliography

  1. Detection and learning of floral electric fields by bumblebees, Dominic Clarke et al, Science, 21 Feb. 2013.
  2. Check out the scientific profile of the petunia
  3. Bees in slow motion!
  4. Bees galore: 50 interesting pics
  5. Find out which flowers attract bumblebees

Warming worries: Wolverine may get endangered status

On Feb. 1, 2013, the U.S. Fish and Wildlife Service proposed adding the wolverine — a tough, reclusive carnivore that lives in the snow in the Rocky Mountains — to the endangered species list. About 300 of these weasel relatives survive amid the heavy snows and severe climate of the high mountains, but global warming is melting their habitat.

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Stance and face give a wolverine the appearance of a small bear as it pads across snow.

Wolverine at an outdoor museum in Skansen, Sweden. Wolverines in the western United States are growing scarce, likely due to a warming climate that is decimating the snowy habitat they require.

The International Union for Conservation of Nature (IUCN) lists 10,820 animal species worldwide. The group’s “Red List” does not distinguish endangered from threatened species.

And now comes the accelerating threat of global warming, a planet-size problem that is sure to make matters worse for rare species in many places and cases. Polar bears and corals have already entered the list of species in danger due to the global changes wrought by greenhouse gases, and more species are doubtless coming, due to changes in precipitation, temperature, disease, ocean acidity, and the timing of flowering, fruiting, migration and the very seasons on our planet.

The Wolverine — no relative of the wolf — is perfectly adapted to the snow, with paws serving as natural snowshoes and dens deep below the snow that are warmed by the lack of wind and insulation from the snowpack. The animals “use snow as a natural refrigerator, caching their food in natural ice boxes,” to sustain them as they bear and nurse their young, says Jonathan Pauli, an assistant professor of wildlife ecology at the University of Wisconsin-Madison. “They are losing this natural refrigerator, which is really problematic because it affects this nutritional pinch point in early spring.”

The wolverine and other snow-dependent mammals are on a collision course with a warming climate, says Pauli. “The winter climate in particular in the Northern hemisphere is changing dramatically. In the last 100 years, we’ve seen an increase of three-quarters of a degree Celsius, and what’s especially relevant is the shortening of the duration and depth of the snow cover. The snow season is being compressed,” he says.

Graph showing average global temperature rising since ~1910; rising above 1901-2000 average in 1970.
The signature of global warming can be traced to about 1980. All of the top 10 warmest years, including 2012, occurred after 1997.
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Furry brown animal, resembling a mix of small raccoon and large ferret, with long tail climbing tree trunk.

Courtesy Jim Woodford
The American marten is a carnivore that spends a lot of time under the snow. Efforts to reintroduce the marten in Wisconsin have faltered, possibly due to a changing climate.

The American Marten is another winter specialist that hunts mice under the snow, but some populations are in trouble. “They are a winter-adapted carnivore,” says Pauli. “They are light and their feet, like the wolverine, are a natural snowshoe” that saves energy. Sinking into deep snow is tiresome and “can put you on the nutritional redline. It’s not just exhausting, it can be deadly.”

The American marten was extirpated from Wisconsin in the 1920s, and reintroduced in the 1950s and again in the 1970s, but they are not prospering, and one possible explanation is the truncated snow season, Pauli says.

Turning turtles

It’s tough to pinpoint the role of a changing climate on endangered species. After all, as pioneering ecologist Barry Commoner said, the first law of ecology is that everything is connected to everything else; nothing exists in isolation. “I don’t know how much hard data there is on a lot of species relative to climate change,” says Scott McRobert, professor of biology at Saint Joseph’s University in Philadelphia. “Although it is probably causing dramatic effects to a large number, it’s hard to isolate climate change from other factors.”

That calculus is evident in the leatherback marine turtles which “have declined exponentially since we started studying them in 1989,” due to hunting of turtles, gathering of eggs, and fishing gear that snared turtles as “by-catch,” says James Spotila, professor of environmental science at Drexel University.

Changing climate is fueling more of the periodic warmings in the central Pacific called el Niño, Spotila says. “When the Pacific warms, there is less [nutrient-rich] upwelling, so the turtles have a harder time getting food,” which impairs growth and reproduction, he says. “Our studies and mathematical model show they will be gravely affected by a changing climate, and it’s starting now.”

Leatherback sea turtles: from eggs to hatchlings

Click to view slideshow.

Leatherbacks and other marine turtles face a second difficulty related to warming: The sex of hatchlings is determined by temperature while the egg develops; when it’s hotter, more females develop. The result is that most turtles developed from eggs laid in January and February are female, says Spotila.

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Hand drawing of finch-sized lemon-lime birds with long, narrow, curved beaks.

Hemignathus procerus, or Kauai akialoa, is endemic to the island of Kaua’i, Hawai’i. The endangered honeycreeper eats insects and sucks honey from tube-shaped flowers. Over two centuries, Hawaiian honeycreepers have suffered many assaults and extinctions. According to a 2011 study, avian malaria is spreading as global warming expands the habitat of its mosquito vector.1 Looking at data on more than 3,000 bird species from seven decades, the authors linked a two- to three-fold increase in bird malaria to about 1°C temperature rise.

On Colombia’s Caribbean coast, 92 percent of leatherbacks are born female in some years, and the temperature anticipated for 2050 will make virtually all of them female. Indeed, a 2012 study.2 warns that “complete feminization could occur, as soon as the next decade.”

Without males, a population crash is inevitable.

Heat by itself is also a problem, says Spotila: “As the season progresses, the hatchlings become weaker and more heat stressed. In April [on Costa Rica's Pacific Coast], there is very low hatchling success due to heat stress.”

Climate change is “a giant bummer,” Spotila says. “We spent 23 years setting up Las Baulas National Marine Park, protecting the beach, and getting a handle on fishing. … The overwhelming effect of global warming is going to make life even more difficult. We are going to see species after species getting these problems.”

Walking that long Amazonian road

In the vast tropical forests that survive in Amazonia, climate change will scourge many habitats, according to a new study.3 Kenneth Feeley, assistant professor of biology at Florida International University, asked how far residents of large ecological situations — biomes — would have to move to find suitable habitat by 2050. “The classic way has been to look at the effect of deforestation or fragmentation as almost one field of conservation biology, and a separate field of climate change ecology,” Feeley told us. “There hasn’t been that much study of both simultaneously.”

Feeley combined these threats. “We looked at the conditions you find in a spot in the Amazon, and asked where would you have go to find the same temperature and precipitation” in 2050, he explains.

And he then blocked off areas that would require traversing large, deforested areas. Already, he notes, many Amazonian animals “are really hesitant to cross a break, a trail, a road or a river,” so requiring animals to avoid deforested areas “shows the true distance that a species has to move.” Large-scale deforestation “creates environmental traps for species, because there is no way to reach the future climate area without crossing a deforested area,” Feeley says.

In many cases, he says, animals would have to travel “off the map.”

Minimum distance to suitable habitat in Amazonia, 2050

Left: Map of Amazon for 2050. most organisms will have to migrate at least 200 kilometers to find suitable habitat.

Right: Map of Amazon for 2050. Most organisms will have to migrate up to 1,000 kilometers to find usable habitat, some find no habitat.

Map at left shows how far species would have to move to find today’s climate after expected changes in temperature and precipitation. Map at right adds in effects of deforestation. Because most organisms cannot cross farm fields, they will have to travel much further to find livable habitat. Organisms now living in the black zones will be homeless.
Both maps used with permission; Feeley and Rehm. Amazon’s vulnerability to climate change heightened by deforestation and man-made dispersal barriers. Global Change Biology. Blackwell Publishing Ltd.

We commented that his maps were profoundly depressing, and Feeley cheerlessly reframed them as best-case scenarios. Organisms, he noted, are inter-dependent: If bird A is needed to pollenate flower B, “that just compounds the difficulties, because both have to arrive simultaneously. And they might depend on a third species. If they do not all arrive simultaneously, it might be impossible for each species to be there.

“The forecast for Amazon biodiversity is really grim,” says Feeley. “Our only hope is that we are wrong.”

What to do?

Scientists are starting to test some tentative fixes for the biodiversity ravages blamed on a changing climate. Many proposals favor preserving more habitat, while choosing more selectively. “We can envisage ways to manage land cover that would mitigate or reinforce the changes we expect,” says Pauli. For example, “Different land-cover types can have a strong effect on ambient conditions in winter; areas with forest cover can have much more moderate temperature than open areas.”

Here are some other ideas we culled from a survey of the changing landscape of hot-world biodiversity preservation:

✻ Mapping migration

The new maps of Amazonia could help in designing migration corridors so species can move as climate changes, says Feeley. “If we know this area will be lost to agriculture, can we plan to place corridors in the most effective places? A lot of the focus in conservation has been on preserving parks, assuming static conditions. Now we are talking more about the need to protect areas to allow species to respond to climate change,” he says.

✻ Change the habitat

Since temperature controls the sex ratio in leatherbacks, Spotila and others are testing whether fresh-water sprinklers and sunshades can cool the beach in Costa Rica to stabilize the male-female ratio and improve hatching success. “We are doing the experiment now, trying to determine which of those options will work,” he says.

Aided by the Climate Adaptation Fund, the Grand Canyon Trust is reintroducing beavers into 87 stream segments in Southern Utah. Rollover to see the change one year later: the new beaver pond has already drowned invasive plants while creating habitat for native plants and animals. Check the video.
First: July 2011, photo by Natalie Jamerson, Whitman College; second: September 2012, photo by Allison Bolgiano, Whitman College

✻ Put wildlife to work!

Beaver dams naturally store water, replenishing aquifers and restoring wetlands for wildlife, while reducing floods and the effects of drought. Now, after centuries of trapping, beavers are returning (via foot or truck) to various landscapes, including the arid Southwest, faced with drought and highly erosive floods in the changing climate.

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With brown-scaled body stretching behind, lizard turns face to the camera with open mouth and outstretched dark blue tongue.

Photo by Peter Shanks
The beautiful blue-tongued lizard, under threat from habitat disturbance and a changing climate, could be moved to better habitat around its native range in southern Australia.

✻ Trucking to a better home?

Moving animals to habitat that remains hospitable in the new climate may be a last resort for animals like the endangered blue-tongued lizard, whose native grasslands in South Australia have been transformed by farmers and now climate change. Some scientists have proposed building artificial burrows for the lizards, and even moving them to new locations where the future’s climate should be more benign. “Although we recognize the importance of conservation efforts to improve the quality, connectivity and permeability of the species’ current habitats, the rapidity of climate change will continue to exceed the ability of some species to adapt or disperse to more climatically favorable regions,” wrote the authors of a 2012 relocation study.4

✻ More shelter from the storm

Captive breeding has been used to sustain whooping cranes and other animals threatened with extermination in the wild, and McRoberts keeps several endangered turtles from Asia or South America in “assurance colonies” in his lab. “At least we can keep some of them alive in the hope that there might be places where they could live in the wild,” he says. As McRoberts recognizes, captive breeding could deflect time and energy from habitat conservation. “Even as someone who does it, I am not saying it’s an optimal way of saving species, but I don’t see it detracting from survival in the wild,” he says. “It’s best to approach any conservation issue from as many different points of view as you can.”

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Two tiny turtles side by side, legs retracted into shells and spotted faces peering out.

Geoclemys hamiltonii, AKA black pond turtle or black spotted turtle, in the McRoberts lab. These threatened turtles eat snails and fish in rivers and ponds with abundant aquatic vegetation in India, Pakistan and Bangladesh.
Courtesy Scott McRoberts, Saint Joseph’s University

Endangered Species Act to the rescue?

Our story started with the potential listing of the wolverine under the Endangered Species Act, a pioneering law premised on the avoidance of extinction. But a 2012 study5 of ESA plans for endangered species in the American West found that “few [climate] adaptation projects have made it to the implementation phase,” due to budget constraints and lack of specific direction from the government agencies involved.

Newer habitat conservation plans should pay more attention to climate, says study author Paola Bernazzani, of the Ohio consulting group ICF International. “There are some good plans coming out in the future, but since we looked retrospectively, there was not anything that did a good job,” she says.

The inability to pinpoint the details of future climate and habitat should not excuse the failure to plan for changes, Bernazzani says. “We admittedly don’t know everything we would like to know to plan for 30 or 50 years, but … the Endangered Species Act was written to anticipate flexibility by calling for adaptive management.”

In a forthcoming plan, Bernazzani says, her company is using computer modeling to explore how fish will move through hydroelectric dams: “We are able to alter the scenarios to fit different climate-change assumptions, and we’ll test them. It’s like a fire drill — you know before implementation what are some potential outcomes.”

Habitat plans may also require establishing preserves to buffer against climate change, Bernazzani says, but the reality is that “we are talking about species that are already rare, and adding one other pressure on top, and I am not sure all the conservation planning in the world is going to solve that.”

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Columns of usually rusty orange coral faded to bright white.

Coral “bleaching” was one of the first recognized biological damages of global warming: When water warms, the coral animals expel the symbiotic partners that feed them, and the coral turns white. Unable to eat, the coral can die if temperatures stay too warm. Bleaching has started in the center of this coral in Indonesia, but coral remains alive around the edges.

The bottom line

Back in the 1980s, climate change was tomorrow’s trouble. Not any more. “There is no question that climate change poses an unprecedented challenge to biodiversity,” says Pauli, the mammologist at the University of Wisconsin-Madison. “It’s one of the biggest conservation crises we are facing.”

To a specialist in winter ecology such as Pauli, the truncation of the snow season “is challenging and frustrating, but it does provide an opportunity to understand the winter system; it’s an experiment that unfolds in real time.”

The reality is that the disruptions due to climate change are seamlessly connected to everything else, says McRoberts. “It’s always very difficult to say a species is encountering difficulty from one direction, and every endangered species is also encountering other problems, habitat destruction being the primary one,” he says.

McRobert agrees that it can be daunting for people who have worked for decades to preserve biodiversity to gird themselves to combat a threat with a global reach. “There are so many issues that you can be overwhelmed easily,” he says. “If you are worried about habitat for endangered species, you should keep working on that” instead of worrying specifically about climate change. “It’s hard to address everything at once.”

David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Bibliography

  1. Climate change increases the risk of malaria in birds, Laszlo Garamszegi, Global Change Biology (2011) 17, 1751–1759, doi: 10.1111/j.1365-2486.2010.02346.x
  2. A potential tool to mitigate the impacts of climate change to the Caribbean leatherback sea turtle, Juan Panito-Martinez et al, Global Change Biology (2012) 18, 401–411, doi: 10.1111/j.1365-2486.2011.02532.x
  3. Amazon’s vulnerability to climate change heightened by deforestation and man-made dispersal barriers, Kenneth J. Feeley et al, Global Change Biology (2012) 18, 3606–3614, doi: 10.1111/gcb.12012
  4. Managed relocation as an adaptation strategy for mitigating climate change threats to the persistence of an endangered lizard, Damien Fordham et al, Global Change Biology (2012) 18, 2743–2755, doi: 10.1111/j.1365-2486.2012.02742.x
  5. Climate change and western public lands … K.M. Archie et al, Ecology and Society, 17:(4) 20, 2012
  6. Slideshow:Great extinctions and great species recoveries featured at the Natural History Museum in London
  7. USGS Scientists answer questions about climate change in the mountains
  8. Who fades first? Pikas: the climate change sentinel species
  9. Worried about trout? See how they fare under climate change preditictions
  10. Hungry for more leatherback facts?

How did the wolf cross the ocean?

It was a mystery of nature even before Charles Darwin reached the Falklands Islands in the South Atlantic: How did the Falklands Islands wolf, the only resident mammal, reach the islands, about 460 kilometers off the Argentine shore?

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Artistic rendering of wolf with penguin between paws

Michael Rothman for Ace Coinage, Inc.
The Falkland Islands wolf was the only mammal on those isolated, South-Atlantic islands until whalers, sealers and farmers exterminated it some time after 1834. A new analysis of ancient DNA shows that it probably crossed a shallow frozen strait during the height of the last ice age, potentially while chasing marine mammals and penguins.

The great naturalist and writer wisely wondered what was weird with the wolf:

“As far as I am aware, there is no other instance in any part of the world, of so small a mass of broken land, distant from a continent, possessing so large a quadruped peculiar to itself,” Charles Darwin, 1834.

After Darwin left, whalers, sealers and farmers hunted and poisoned the Falklands wolf to extinction.

Nobody thought the wolf, AKA Dusicyon australis, had crossed the strait. Did it cross on a raft made of trees, walk on the winter ice, or catch a ferry ride from obliging people now lost to history?

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Map of Falkland Islands--superimposed and called out from image of earth.

When Charles Darwin collected a wolf specimen on the Falklands Islands in 1834, he wondered why no other species of mammal lived on the remote islands. Now we know.

The question of colonization of remote islands recurs often in natural history: The journeys of plants, parasites, people and other mammals beg for explanation, especially on remote islands like the Falklands.

Now, a team from the University of Adelaide in Australia has combined forensic genetics with paleogeography to come up with an answer, based on shifting sea levels and the wolf’s relationships to relatives on the mainland.

Welcome the newbie!

The study began by analyzing genetic sequences to identify when the Falklands wolf split off from its last common ancestor, a now-extinct mainland fox called Dusicyon avus. Logically, the wolf made its crossing after it diverged from its ancestor.

Instead of dating the fork in the road with standard rates of mutation, the researchers carbon-dated the ancestor’s remains. After counting the genetic differences between the wolf and the fox, they arrived at a rate of molecular changes per year for those animals, at that time, says senior author Alan Cooper of the Australian Centre for Ancient DNA. “We think this is a much better approach than standard mutation rates. This is quite an important difference from other studies.”

Previously, scientists concluded that the wolf had reached the Falklands about 330,000 years ago, but the new analysis — focusing on a different last common ancestor — pointed toward a much more recent arrival, about 16,000 years ago.

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ged notebook page with many names and addresses in elegant inked writing

I got Darwin’s address! says Alfred Russel Wallace, who mailed a manuscript to Charles Darwin in 1858, prodding the elder naturalist to hurry up publication of his theory of evolution, which he’d been working on for 20 years.

That was during the height of the Wisconsin ice age, when ice sheets, especially on Antarctica, locked up ocean water, causing sea level to fall. That exposed “land bridges” linking islands and continents.

As the ocean surface declined about 130 meters, the strait separating the Falklands (known in Argentina as the Malvinas Islands) narrowed to a couple of dozen kilometers. Presumably this water froze during some winters, and the wolf either roamed across or rafted on icebergs.

It’s possible that other mammals reached the Falklands but left no traces — or that the wolf was the only mammal to cross the strait. “The wolves were after marine resources, like seals, penguins and seabirds, on the edge of the ice,” says Cooper. “Other mammals such as rodents, which are common in South America, were not interested in crossing 20 to 30 kilometers of ice, as there is no food or habitat.”

I go, you stay

The study brings into focus the role of climate and sea level in colonizing remote islands. “Strangely enough,” says Cooper, the role of sea level change “was the key observation that led Alfred Russel Wallace to discover evolution independently from Darwin.”

In 1858, Wallace, a naturalist, mailed his theory of natural selection to Darwin, who recognized it as strikingly similar to his own, unpublished theory. Darwin helped arrange a simultaneous reading of the theories at a scientific meeting in 1859.

Wallace, who was still collecting specimens in the southwest Pacific, noted that similar animals lived on islands that were separated by shallow seas. But when he looked at organisms on opposite sides of what’s now called the “Wallace line,” he saw that animals like those in Australia lived to the east. The animals living to the west were related to those living in Asia.

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Map of South Pacific islands with line through Indonesia separating east and west.

Wallace, pioneering student of the geography of natural history, realized that this line marked a major distinction in animals. Marsupials were common to the east and south, while animals with placentas were common to the north and west.

And dividing the two regions is the Lombok Strait, which was deep enough to remain open during glacial times, and too warm to freeze over, even during the Ice Ages. Although Darwin is rightly credited as the originator of evolution through natural selection, “he didn’t really seem to grasp the role of sea level change to the same degree,” says Cooper.

But let’s give Darwin the last word: The Falklands wolf DNA used in the study came from a specimen Darwin collected in 1834.

— David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Bibliography

  1. The origins of the enigmatic Falklands Islands wolf, Jeremy Austin et al, Nature Communications, 5 May 2013.
  2. Looking for lost letters between Darwin and Wallace
  3. The Darwin Correspondance Project
  4. Learn about the HMS Beagle, Darwin’s adventure ship!
  5. Wallace & Darwin: Friends or Foes?
  6. A naturalist’s notes: Wallace’s original journal

Space rocks falling down. Time for a meteorite hunt?

The biggest meteorite in a century struck Chelyabinsk, Russia, on Feb. 15, when an asteroid about 55 feet (17 meters) across, with a mass of 10,000 tons, exploded in the upper atmosphere. The explosion and fireball released about as much energy as a 500-kiloton atomic bomb — 30 times more than the bomb that devastated Hiroshima in 1945.

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Long, narrow cloud streaks across entire horizon, angled downward to Earth.

This is the meteor that flew over the Urals early on the morning of Feb. 15, 2013. The fireball exploded above the city of Chelyabinsk, damaged dozens of buildings and injured hundreds of people. This photo was taken about 200 kilometers away, about a minute after the photographer saw the blast.

Shock waves through the atmosphere caused widespread destruction. Flying glass from thousands of broken windows was the major cause of an estimated 1,200 injuries.

But as the physical and emotional shock wore off, residents began collecting fragments. Soon, as happens after any substantial meteorite falls, professional meteorite hunters and go-betweens were buying fragments of space rock from locals.

Background image from photo by David Kingham

Twenty five years ago, this would not have happened, but both amateur and professional interest with meteorites has exploded, says Geoff Notkin, co-host of the cable TV show Meteorite Men. “I have been in the field for almost 20 years, and when I first got interested, there were only a handful of people, other than a few academics. Now there are thousands of collectors worldwide, a couple of popular publications, our TV show, high profile auctions and a number of new books.”

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Man on dull orange vegetation-less landscape holding two long metal detectors.

Courtesy Geoff Notkin
Geoff Notkin, one of TV’s “Meteorite Men,” searches for rocks from the sky in Chile’s ultra-arid Atacama Desert.

Much of the surge in popularity can be credited to the Internet. “In the pre-Internet age, meteorite collecting was a small hobby, and meteoritics a comparatively small science. It was difficult to connect,” says Notkin. “There was no magazine, no forum. You might meet someone at a rock show, but there was no network of collectors and enthusiasts.”

The sale of major fossils to private collectors often sparks a chorus of scientific caterwauling, concerned that scientists will be barred from private storehouses sequestering significant samples of natural history. Do professional meteorite hunters and the market they feed harm science even as they cater to people who covet chunks of ancient space?

Certainly, the motivations of scientists and collectors overlap, says Ralph Harvey, associate professor of planetary materials at Case Western Reserve University. “You would not be a private meteorite collector or a meteorite scientist if you were not jazzed about stuff that falls from space. That’s clearly what we have in common.”

But motivations vary widely in the private world, Harvey adds. “Plenty of people cross the boundary well, are part collectors and part scientists. The big difference arises with people who focus on specimens as much from a financial as a scientific or curiosity point of view.”

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Glass case holding an array of meteorite specimens

Great collections like the one at the Smithsonian Museum of Natural History set the standard for meteorite displays — and also raise the price of the rarest, most astounding examples.

Chelyabinsk, Russia, was a “fireball for the ages,” says Harvey. “My sympathies go out to the people who were hurt… but I would love to have witnessed that fireball from a safe distance. It’s awesome. Dangerous but awesome.”

The oldest text?

Meteorites formed as the solar system coalesced from the primordial cloud of dust about 4.56 billion years ago. Since then, their surfaces have gathered dust, and many have suffered a gigantic collision with another asteroid. In the last few seconds of their lives, they get a black “fusion” crust as they burn through the atmosphere.

Nonetheless, meteorites are unchanged in comparison to rocks on Earth, which have been altered by squeezing, heating and chemical reactions over the eons. And that makes these messengers from the deep solar system deeply important to science.

Some meteorites are not just time capsules from the ancient solar system: the most intriguing space rocks were blasted from the surface of the moon or Mars by asteroid impacts. “They are our only tangible samples of material from Mars,” says Carl Agee, director of the Institute of Meteoritics at the University of New Mexico.

Agee says even rarer meteorites — blasted from Mercury or Venus — could be lying on some farm field or ice sheet, awaiting discovery.

As meteorite hunters continue to harvest a growing roster of rocks, scientists hunger for more, says Harvey. “Meteorites are still really rare. If you looking for an answer to where it all came from, it starts with meteorites, but we have a few tens of thousands of pieces [representing] an entity as big as the solar system. The rocky inner planets have been changing for billions of years, Harvey notes, so “The only way you can get at the original conditions is in these bits and pieces that were hidden in a corner of the solar system.”

Meteorite hunting, 21st century style

Meteorite hunting has transcended the “farmer finds weird rock” phase, Harvey says. “Before 1950, virtually all of them were found by farmers in fields, maybe they were plowing and hit something, or saw it fall and rushed over to pick it up. Later, most were recovered because they hit a building, a car or a road. In the last five to six years, most are now found after being seen on a video camera or other monitoring system,” such as weather radar.

Shiny silver rock rests on metal disk in gloved hand.
Noriko Kita, director of the Ion Microprobe Laboratory at the University of Wisconsin-Madison, removes a piece of rock, believed to be from the April 14, 2010 Mifflin meteor in Southwestern Wisconsin, from a scanning electron microscope. The fragment was found by a Wisconsin farmer and brought to the university for analysis.

After a big fireball, hordes of meteorite hunters are likely to descend on the impact zone, and they now use technology to find elusive rocks hiding across a broad landscape, says Richard Slaughter, director of the Geology Museum at the University of Wisconsin-Madison.

Slaughter, who tried his hand at meteorite hunting after a strike in Wisconsin in 2010, says hunters “have online forums and list serves; they are very strategic.” The majority of finds on a “strewnfield map” came from meteorite enthusiasts, not scientists, Slaughter says. “They are very systematic, use all the data to find the best places to look.”

Radar records and metal detectors are standard techniques to combat the “needle in haystack” problem. Metal detectors, Notkin says, are most useful for iron meteorites (typically about 93 percent iron) and stony-iron meteorites (about 50 percent iron). Detectors will also detect the more common stony meteorites, typically containing about 20 percent iron, but with more difficulty.

The Polar solution

Laws governing the collecting of meteorites vary widely, but they are unambiguous in Antarctica, where the scouring wind leaves dark space rocks exposed on the snow. Because the Antarctic treaty forbids private ownership of rock or ice samples, the U.S. Antarctic Search for Meteorites program, now in its 35th year, delivers meteorites to NASA, which catalogs and distributes them to scientists who can make a convincing case for their need.

Two silhouetted figures on icy landscape with many dark rocks protruding through white snow.
Though these rocks are probably not meteorites, the contrast between rock and ice is written in black and white. The Antarctic survey team frequently retrieves more than 100 meteorites in a day.

Harvey, who directs the Antarctic search program, says its founder William Cassidy, “knew that the meteorites would have such impact on science that we should give the samples away and not lay any claim on them. It’s as if a scientist walked through the Brazilian jungle and found a lost civilization, and said, ‘Let me call the 50 best people to investigate, and I’ll step back.’ It’s incredibly altruistic.”

At the other extreme, meteorites in the United States belong to the owner of the land they smash into. In 2012, the U.S. Bureau of Land Management issued new rules that permit “casual collection” on BLM land, but require a permit for commercial and scientific collectors.

The human element

The growing number of people who march, heads down, across the landscape after a fireball are not always easy to categorize. Some are focused on making money on what they find, but most are probably “meteorite enthusiasts, the true collectors who end up spending money on meteorites, not making it,” says Agee. However, some collectors are happy to sell when the opportunity arises, and meteorite dealers may also hunt.

We mused that the meteorite hunters could be the modern counterparts of the lone-wolf prospectors, who, with pick and mule, sought gold, silver and uranium in years past. Not so, says Slaughter. “There are handfuls of professionals, and they are very knowledgeable, and much more high-tech than the old prospectors.”

The hunters differ in another respect, says Slaughter. “I think it’s actually a much more social endeavor than the loner with his mule. You want to know who is looking where, what they are finding, how it compares to what you are finding.”

Meteorites land all over the place, Slaughter says, “so you need to know how to communicate in multiple languages, be aware of different legalities. Going up to the landowner and trying to get permission to look on the land is a surprisingly human exchange. When you are out looking with a team and you’re exhausted, dealing with that requires a human element.”

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Tweezers hover over graph paper holding array of small rock chips.

Meteorite chips from the recent Chelyabinsk meteorite under analysis at a nanomaterials laboratory at Ural Federal University in Russia.

A surprising synergy

We went into this story wondering about a tension between the business of meteorites and the science of meteoritics, but we came out reassured. Are private collectors hiding meteorites from science? “I hear that rap in lots of areas: fossils, minerals and meteorites,” says Slaughter of the Wisconsin Geology Museum, “but I think actually in the meteorite world, scientists and collectors have worked out a mutually beneficial arrangement.”

The scientists who study meteorites often work at universities, and classes and students make it awkward to buy a ticket after a fireball has lit up some remote location. “Working with collectors is certainly the most cost-efficient way to get pieces,” says Slaughter, “and we don’t need very much to do the analysis, a few grams is usually a treasure trove.”

Agee, who is also professor of earth and planetary sciences at the University of New Mexico, agrees, “I have good interactions with collectors. Some of them put together really impressive collections that are on a par with museum collections, and often the collectors are keen to interact with the scientific community. A number of collectors I work with have donated to museums.”

But there are exceptions, Agee adds. “Like any business, you have people who are better citizens than others. It’s a reflection of the real world.”

“There are meteorite collectors who are every bit as zealous as those who collect art, prehistoric artifacts, or anything, really,” says Harvey. “When you have a fever for that kind of stuff, and part of the reason is financial, there are collectors out there — it’s a very small percentage — who, for lack of a better word, have bent the rules, had brushes with the law.”

Daddy’s meteorite

The publicity surrounding meteorites can actually pull samples off the woodwork, says Notkin. The “Sterley pallasite,” for example, sat for six decades on the family mantelpiece, but when it was analyzed at the Center for Meteorite Study at Arizona State University, it was recognized as one of only 86 known pallasite meteorites.

Photo by Suzanne Morrison © Aerolite Meteorites, LLC
The Sterley pallasite was discovered about 1950 by a Texas farmer, but was not classified or analyzed until 2012 when the finder’s family saw an episode of “Meteorite Men” on television. Pallasites are composed of approximately 50 percent nickel-iron and 50 percent olivine. Roll over photo for a detail of a full slice after preparation; the translucent areas are olivine crystals.

Notkin’s business, Aerolite, bought the meteorite, donated part to Arizona State, which had done the classification, and distributed parts to six researchers worldwide. “This meteorite turn out to be completely new and extremely rare, it’s one of the most beautiful ever found,” says Notkin.

The ability to contribute to significant research collections is a major motivation for amateurs, Notkin adds. “Amateur does not mean ignorant. In this scientific field, a lot of the most important contributions have been made by amateurs. As the word suggests, they do it for love, not for a stipend.”

Still, when it comes to the large, dramatic samples that museums want to grab eyeballs, the free market can impinge on short-budgeted university museums. Slaughter, for example, recently attended the Tucson Gem and Mineral Show, seeking a piece of a Martian meteorite, but the prices approached $1,000 per gram, and the University of Wisconsin Geology Museum had to decline.

At this point, the rising interest in the rocks arriving from space, among amateurs and professionals, is reinforcing our understanding of the evolution of the solar system. “We are about where the biology of natural selection was 200 years ago,” says Harvey. “Not too many years go by without the equivalent of another platypus coming along that does not fit our understanding of how meteorites relate to each other and to their parent body.”

– David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Bibliography

  1. Meteorite Hunting: How to Find Treasure from Space, 96 pp. Geoffrey Notkin, 2011.
  2. Up close with metoerites
  3. Antarctic meteorites reveal solar system history
  4. One man’s $5 million meteorite collection
  5. Photo: the huge, goregeous Fukang meteorite
  6. What does it look like to search for meteorites in Antarctica? Like this!
  7. Meteorite collector proudly poses with specimen

 

2013 Cool Science Image Contest

Click to view slideshow.

 

Congratulations to our winners!

Scientific imagery, of course, is intended to help scientists. It is a critical form of data in many fields and can yield important and sometimes striking insights into nature and the way things work.

But the pictures and other images of science can also have remarkable aesthetic qualities that the non-scientist can appreciate. That has been the philosophy of our Cool Science Image feature, published on this site for 17 years.

promega logo

Three years ago, as an experiment, The Why Files held its first Cool Science Image contest. Limited to Why Files headquarters, the University of Wisconsin-Madison, the contest yielded more than 60 entries.The next year 84 Badgers entered the competition. This year, there were 105 submissions. This year also sees a new sponsor for the contest. We welcome the interest and generous support from Madison-based Promega Corp.

Choosing the winners was difficult, but our judges narrowed the field to ten winners, included in this slide show.

The experiment, we think, has been a success. Our goal now is to continue this as an annual event. We hope to grow the contest and help bring the visual beauty of science to a larger audience, an aspiration that can make all of us winners.

*If you wish to repost any of these images, please acknowledge the University of Wisconsin-Madison and include a link to this site. We would also appreciate notification of repostings.

Getting on the high road?

Do you love roads or hate them? If you’re an environmentalist, chances are you’re at least highly skeptical. Roads are famous for bringing settlers, forest destruction and farms to natural areas that are often inappropriate for sustainable agriculture.

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Brown dirt road passing small home and cutting through treed area.

Near Manaus, Brazil, Photo: Julio Pantoja / World Bank World Bank Photo Collection
In the Amazon basin, locals harvest forest products like mandioca, coconuts and cocoa to eat and sell.

But the agricultural industry, and people who promote farming as an antidote to hunger and poverty, see another side to roads. Farmers who want to do more than feed their families need good roads to bring in advisors, fertilizer and seeds, and take crops to market.

Roads that are muddy or impassable can make transport so expensive that cash cropping makes no sense.

This week, the journal Nature prints a proposal to square this circle by developing a system to chart where roads are beneficial, and where they are harmful. As the authors wrote, “We propose that environmental scientists, planners, road engineers and other stakeholders carry out a global ‘road-zoning’ project to map areas that should remain road-free and those in which transport urgently needs improving.”

We emailed corresponding author William Laurance, a conservation biologist at James Cook University in Australia, to ask if the idea was “pie in the sky.” Not so, he wrote. “What we’re hoping to see produced is a tool that anyone can use to prioritize where and where not to put roads. Some stakeholders and nations will hopefully use it, but of course not everyone will.”

Roads and forest degradation in Rondônia (western Brazil)

The forest in the state of Rondônia was once almost as big as Kansas, at 208,000 square kilometers. According to the Nature study, more than 95 percent of deforestation, fires and atmospheric carbon emissions in the Brazilian Amazon occur within 50 kilometers of a road. Intact forest is deep green, cleared areas are tan (bare ground) or light green (crops, pasture, or occasionally, second-growth forest). Between 2000 and 2009, deforestation in the state grew from 30,000 past 51,000 square kilometers. Rollover to see the change by 2009.
Images: MODIS/Terra, NASA Earth Observatory

Although rampant road-building in tropical forests has lead to significant forest destruction, “The situation is slowly improving,” Laurence wrote to us.  “Big highways tend to be more controlled than secondary and tertiary roads. Many of these smaller roads are being created illegally in remote areas, and that’s something that needs to be cracked down on.”

“We’re hoping to see a tool that anyone can use to prioritize where and where not to put roads.”

Roads really matter, says Lisa Naughton, a professor of geography at the University of Wisconsin-Madison, who studies development and conservation in the tropics. When the Interoceanic Highway was recently completed in the Peruvian Amazon, she says, “It utterly transformed the relationship between people, land and forests. The long-term efforts of Peruvian conservationists to promote sustainable agroforestry and non-timber forest-product harvest (such as Brazil nuts) were rapidly undermined as the road brought in large-scale agriculture, and deforestation has accelerated.”

Building in the zone

Rather than establish mandatory zoning, Laurance envisions a map that helps planners, politicians, agricultural interests and conservationists guide development while protecting indigenous lands, biodiversity hotspots and other sensitive areas.

The balanced approach, he says, “is a potential advantage … . We’re not saying to simply stop all road building. We’re saying let’s stop some of the environmentally destructive roads … while at the same time focusing road building where it’s likely to have the biggest economic and social benefits.”

According to projections, the demand for food will soar by 2050, due to a rising population with a growing desire for meat. According to the Laurance study, an extra 1 billion hectares (which happens to be the size of Canada!) will be needed for crops and grazing land. Much of that will have to take place on wild land.

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Food consumption and population increase in parallel through 2050.

Consumption of cereals — primarily maize, wheat, rice and soybeans — is expected to soar along with continued population growth and prosperity.

But boosting agricultural productivity could supply some of this food, slowing the destruction of wild lands and wild creatures.

Roads: Farmers’ best friend?

It’s impossible to imagine advanced agriculture in developed countries without good roads. Do roads play the same role in developing nations? “It’s funny—this is one of those ideas that seems to be widely accepted but doesn’t have a lot of formal evidence,” wrote Laurance. “I know because we’ve looked. … In scientific terms, there is a scattering of papers and books that use econometric approaches to argue that road improvements benefit agriculture — reducing waste, increasing market access and improving profitability. But … there doesn’t seem to be much debate about this among those who study such things.”

ENLARGE

Photo shows person on loaded bike riding along muddy road that sweeps uphill and to the left, in the midst of a grain field.

Photo: © Curt Carnemark / World Bank Photo Collection
Roads like this one in Morocco are not conducive to modern, profitable farming. Could better roads help local people while reducing the pressure on wild lands?

Even if zoning for roads makes sense, practically speaking, could it work? Although national governments “have legal sovereignty over their lands, there are very powerful economic forces at work to promote road building — some of which are clearly inadvisable environmentally,” Laurance responded. The road-zoning scheme “could be used by governments and also conservation groups and other stakeholders to facilitate road planning.”

“The call for ecologically-informed road zoning is appropriate but faces major political challenges,” says Naughton, director of the Land Tenure Center at UW-Madison. “Perhaps some of the major roads funded by multi-lateral development agencies can be planned to lower social and biodiversity impacts. But there is ever more private and unilateral international funding available for road-building. More fundamentally, road-building has great political importance in a place like the Amazon — even if a road makes little economic sense, there are often strong political incentives to build it.”

But Laurance notes that, in the face of a proposal to push a road through a wilderness, “With a good road-zoning scheme, you could say, ‘Hold on a minute — that’s an environmental red-zone, the last place you’d want to construct a road. Let’s consider another route or perhaps even forego a new road altogether. Roads profoundly influence the spatial footprint of human activities, and so it’s crucial to focus explicitly on them.”

— David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Bibliography

  1. A global map for road building, William F. Laurance and Andrew Balmford, Nature, 21 March 2013.
  2. The power of rural infrastructure for developing nations
  3. Deforestation in the Amazon: Satellite timelapse
  4. The Amazon Road: Paving Paradise For Progress?
  5. From nothing to nowhere? A different take on the Amazonian highway
  6. Global food demand: Get the facts!

Man swallowed by sinkhole, dies in Florida

On Feb. 28, 2013, the earth opened up in Seffner, Florida, and Jeffrey Bush fell to his death. Local authorities decided they could not safely recover the body: excavating the rock and sand would cause more collapse and more danger.

Man's face crumpled in grief.
Photo: Daily News
Jeremy Bush, who tried to save his brother, Jeff, says his parents are ‘going through hell’ after Jeff died in a Florida sinkhole Feb. 28.

Then, on March 12, an Illinois golfer fell through a sinkhole — possibly associated with an abandoned mine — on the 14th hole. Mark Mihal, 43, survived an 18-foot fall with just a sore shoulder, after his golfing companions fished him out with a rope.

ENLARGE

House that is partially caved into ground with large cracks through roof.

Photo: 2009, Richard Elzey
This house suffered severe damage in Brooksville, Fla., 50 miles north of Seffner, site of the recent tragedy.

The incidents are graphic examples of the dangers of taking geology for granted. Earth is not always as solid as a rock.

In large parts of Florida and other states, a soluble subsurface geology called karst is conducive to sinkholes. Karst occurs in rock dominated by gypsum, limestone or salt — which can dissolve, leaving underground streams and cavities.

The U.S. Geological Survey says about 20 percent of the United States overlies karst terrain; the worst sinkhole damage occurs in Florida, Texas, Alabama, Missouri, Kentucky, Tennessee and Pennsylvania.

Classically, sinkholes occur in locations where water, unable to flow laterally, percolates through soluble rock, creating caverns and cavities. Often, the surface will gradually subside, causing a cover-subsidence sinkhole. And as we’ll see, other forms of collapse are popularly called sinkholes as well.

Cover subsidence sinkhole

Sinkhole forming as overlying land slowing erodes downward to fill underground hole.

Gradual movement of soil grains into cavities in karst can result in a widespread form of sinkhole that is damaging, but not especially dangerous.

More rarely and dramatically, when the roof span becomes too large, the outcome is a “cavity collapse” sinkhole. That was apparently the fatal flaw in Seffner, Fla.

Cover collapse sinkhole

Sinkhole forms suddenly after underground sediment layer between land surface and underground cavity thins.

The undetectable underground changes can take centuries, until the earth gives way with a sudden, dangerous collapse.

Subsidence can also occur

Above mines and underground streams

In organic soils that shrink when they decompose

After routine activities like pumping groundwater up for drinking and irrigation, which removes water from an aquifer and reduces the volume of sand and gravel, causing subsidence

In cold winters in the strawberry fields east of Tampa, Fla., farmers pump groundwater so they can spray their crops to prevent freezing. “In 2010, this opened about 140 sinkholes,” says Mark Stewart, professor of geology at the University of South Florida. “Most of them did not damage homes, but several did, and there was some damage to an interstate highway.”

Sinkholes in Florida

Cover-collapse sinkholes found in Panhandle, near Tampa, and in Northeast Florida.

Modified from original map by Florida Geological Survey
Cover-collapse sinkholes dominate in the blue and purple regions.

Because wells are a known trigger for sinkholes, many subdivisions in the sinkhole-prone North Tampa area prohibit private wells, Stewart says. “You can’t have a well for irrigation or water supply. You have to be on city water.”

The many sides of subsidence

Guatemala City sinkhole: 2010

Photos: 1.) horslips5, 2.) horslips5
At least one man was killed after a three-storey building fell into this 200-foot-deep hole after Tropical storm Agatha dumped more than three feet of rain on Guatemala. Rollover to see a street-level view.

If removing water can cause collapses, so can adding water through leaking water pipes, sewers and storms. Storm runoff was blamed for a dramatic hole-in-the-ground that formed in Guatemala City, Guatemala, in 2010. The city is built on a volcanic ash plateau, and groundwater, sewer systems and storm drains all feed the fragile ash. “The result is erosion of the material, which creates cavities that can collapse,” says Stewart. “It can be really catastrophic.”

In New Orleans and other river deltas, subsidence occurs as organic material in soil decomposes and new sediment, which would sustain ground level, is blocked behind levees. Parts of the Sacramento-San Joaquin river delta in California have fallen to more than 15 feet below sea level.

Sinkholes can result when industrial and water-storage ponds get so heavy that they trigger a collapse.

Large diagram of landscape shows different subsidence risks after mining.
Pennsylvania, riddled with expired coal mines, has major problems with subsidence.

Minding mining

And then there is mining, which is a major cause of subsidence in Pennsylvania, West Virginia and Kentucky. Those states have about 60 percent of U.S. abandoned coal mines; overall, the nation has about 14,000 active mines, and up to 500,000 abandoned mines of all sorts.

Asphalt road with chasm; half of road has sunk several feet Finding that sinking feeling.
A collapse at the Retsof mine in Upstate New York had broad repercussions for the economy, landscape and groundwater.

In 1994, an earthquake collapsed a 500-foot square chunk of roof rock above a huge salt mine south of Rochester, N.Y., and water began flooding in. Since the Retsof mine opened in 1885, it had grown into the world’s second-largest salt mine, covering 10 square miles.

Within 21 months, the mine was inundated and closed. Water levels dropped in wells as far as 10 miles away, and two sinkholes formed, each about 50 by 200 feet. Further subsidence is expected as groundwater dissolves more salt; eventually, as the mine roof continues its slow-motion collapse, the ground above the mine is expected to fall eight or nine feet.

ENLARGE

Corner of house with long horizontal crack from foundation to doorway.

A telltale of subsidence. Don’t buy this house ’til you find out what caused that nasty crack!

Finding that sinking feeling

Sinkholes can be surprising, but they don’t appear at random. In sinkhole-prone states, state geological survey maps should provide at least a general guide to risk; the USGS also has a national mapping facility.

Although a cover-collapse sinkhole may come without warning, experts say people in karst terrain should look for these signs of subsidence:

Cracks in the walls and foundation

Doors and windows that refuse to close

Settling around the foundation

Recognizing safe building sites in areas prone to sinkholes entails a multipronged approach, writes sinkhole expert Francisco Gutiérrez, professor of geology at the University of Zaragoza, Spain.

Identification techniques include field surveys and geomorphological mapping combined with accounts from local people and historical sources. Detailed sinkhole maps can be constructed from sequential historical maps, recent topographical maps, and digital elevation models complemented with building-damage surveying, remote sensing, and high-resolution geodetic [Earth-measurement] surveys. On a more detailed level, information from exposed paleosubsidence features (paleokarst), speleological [cave] explorations, geophysical investigations, trenching, dating techniques, and boreholes may help in investigating dissolution and subsidence features. Information on the hydrogeological pathways including caves, springs and swallow holes [where streams disappear belowground] are particularly important … .1

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Expanse of rocky cliff showing many holes and large hollows.

Photo: Minerve, Hérault Department, France, Wikimedia Commons
This karst landscape shows how water carves conduits and cavities in limestone and other soluble rock. The river through the village of Minerve in southern France disappears into a swallow hole in the karst below town!
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1967 newspaper headline with map of Florida showing sinkhole locations.

The New York Times
Sinkholes are nothing new around Tampa.

Yet as the recent Florida case shows, cover-collapse sinkholes usually come out of the blue. You might think that a state laced with sinkholes would want to zone development away from danger, but the Florida Board of Realtors “is not interested in any kind of hazard zoning,” Stewart says. “To get a mortgage, you must have homeowner’s insurance, and then it would be extraordinarily difficult to get insurance, so banks would be very hesitant to give mortgages, and that would greatly affect property values” in sinkhole areas. Rather than blacklisting areas likely to subside or collapse, the trend is to “leave the risk to the homeowner.”

Better take out some insurance

The Florida insurance industry, buffeted by sinkhole claims, has pushed through a law requiring cases to be settled by arbitration, rather in court, Stewart says. “There was a substantial loss to the insurance industry, so the legislation was changed.”

ENLARGE

Several people stand, looking at chasm in grassy field along road.

September 2003, U.S. Geological Survey
This cover-collapse sinkhole occurred in limestone near Frederick, Maryland. Many sinkholes occur along highways where rainwater runoff concentrates in storm drains and ditches and erodes the subsurface. That storm sewer pipe may have played a role in creating the sinkhole.

Homeowner’s insurance in Florida does cover sinkholes, he says, but not other causes of subsidence, which can cause slow-mo damage. Insurance companies “typically call in a geotechnical firm to do an investigation. In many, many cases, it’s not due to a sinkhole, so the homeowner hires their own geotechnical firm, which says it is, and the issue goes to arbitration.”

One source of data, ground penetrating radar, which reflects off different layers in the subsurface, “can be interpreted over a broad range by experts,” says Stewart. “The level of professionalism among people in the industry has not been at its highest level. Until recently there was a lot of money to be made by lawyers, geotechnical firms and the insurance industry.”

In 2010 alone, there were more than 6,600 sinkhole claims in Florida, Stewart says. “It’s not possible to estimate how many were legitimate. There are geotechnical experts on both sides, so there is no final determination whether it was a sinkhole.”

In a sense, sinkholes, like lightning are frightening natural phenomena that seem to strike from nowhere. “A hole opened under the bedroom and the man went down and was buried while sleeping,” says Stewart. “The Earth isn’t supposed to open up under you. It’s like shark attacks; they get press even though they are extraordinarily rare. Because of the emotional attachment, people see too much risk where there is in reality low risk.”

– David J. Tenenbaum

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Terry Devitt, editor; S.V. Medaris, designer/illustrator; David J. Tenenbaum, feature writer; Amy Toburen, content development executive; Emily Eggleston, project assistant

Bibliography

  1. Identification, prediction, and mitigation of sinkhole hazards in evaporite karst areas, F. Gutiérrez et al, Environ Geol (2008) 53:1007–1022
  2. Sinkholes
  3. In the news: Florida’s sinkhole problems
  4. USGS’s take on the science of sinkholes
  5. Florida’s sinkhole geology
  6. 12 amazing holes in The Earth
  7. What happens after mines close?