Snowball Earth: The Story of a Maverick Scientist and His Theory of the Global Catastrophe That Spawned Life As We Know It Kindle Edition
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Editorial Reviews
From Publishers Weekly
Part biography and part scientific detective story, this debut by British science journalist Walker (a features editor for New Scientist) tells the story of Paul Hoffman, the brilliant, cantankerous Harvard geology professor most responsible for promoting the concept of "Snowball Earth." This controversial hypothesis asserts that about 600 million years ago, the entire planet was encased in ice that was thicker and lasted millennia longer than in any previously recognized ice age. Instantaneously in geologic time, the hypothesis continues, the planet moved from temperatures averaging minus 40 degrees centigrade to sweltering heat unlike anything seen since. These extreme climatic fluctuations may have been responsible for the origination of multicellular life at the beginning of the Cambrian Era and thus, ultimately, for most life on Earth today. Walker does a superb job of relating both the scientific and the human side of the controversy. Her prose, like her story, is likely to engage both scientists and general readers equally. All will be able to appreciate the importance of the issues while gaining greater insight into the process of scientific advances. Walker has written an important, provocative book that is a joy to read.
Copyright 2003 Reed Business Information, Inc. --This text refers to an alternate kindle_edition edition.
Copyright 2003 Reed Business Information, Inc. --This text refers to an alternate kindle_edition edition.
From the Inside Flap
Did the Earth once undergo a super ice age, one that froze the entire planet from the poles to the equator? In Snowball Earth, gifted writer Gabrielle Walker has crafted an intriguing global adventure story, following maverick scientist Paul Hoffmans quest to prove a theory so audacious and profound that it is shaking the world of earth sciences to its core.
In lyrical prose that brings each remote and alluring locale vividly to life, Walker takes us on a thrilling natural history expedition to witness firsthand the supporting evidence Hoffman has pieced together. That evidence, he argues, shows that 700 million years ago the Earth did indeed freeze over completely, becoming a giant snowball, in the worst climatic catastrophe in history. Even more startling is his assertion that, instead of ending life on Earth, this global deep freeze was the trigger for the Cambrian Explosion, the hitherto unexplained moment in geological time when a glorious profusion of complex life forms first emerged from the primordial ooze.
In a story full of intellectual intrigue, we follow the irascible but brilliant Hoffman and a supporting cast of intrepid geologists as they scour the planet, uncovering clue after surprising clue. We travel to a primeval lagoon at Shark Bay in western Australia, where dolphins cavort with swimmers every morning at seven and living rocks sprout out of the water like broccoli heads; to the desolate and forbidding ice fields of a tiny Arctic archipelago seven hundred miles north of Norway; to the surprising fossil beds that decorate Newfoundlands foggy and windswept coastline; and on to the superheated salt pans of Californias Death Valley.
Through the contours of these rich and varied landscapes Walker teaches us to read the traces of geological time with expert eyes, and we marvel at the stunning feats of resilience and renewal our remarkable planet is capable of. Snowball Earth is science writing at its most gripping and enlightening.
From the Hardcover edition. --This text refers to an alternate kindle_edition edition.
In lyrical prose that brings each remote and alluring locale vividly to life, Walker takes us on a thrilling natural history expedition to witness firsthand the supporting evidence Hoffman has pieced together. That evidence, he argues, shows that 700 million years ago the Earth did indeed freeze over completely, becoming a giant snowball, in the worst climatic catastrophe in history. Even more startling is his assertion that, instead of ending life on Earth, this global deep freeze was the trigger for the Cambrian Explosion, the hitherto unexplained moment in geological time when a glorious profusion of complex life forms first emerged from the primordial ooze.
In a story full of intellectual intrigue, we follow the irascible but brilliant Hoffman and a supporting cast of intrepid geologists as they scour the planet, uncovering clue after surprising clue. We travel to a primeval lagoon at Shark Bay in western Australia, where dolphins cavort with swimmers every morning at seven and living rocks sprout out of the water like broccoli heads; to the desolate and forbidding ice fields of a tiny Arctic archipelago seven hundred miles north of Norway; to the surprising fossil beds that decorate Newfoundlands foggy and windswept coastline; and on to the superheated salt pans of Californias Death Valley.
Through the contours of these rich and varied landscapes Walker teaches us to read the traces of geological time with expert eyes, and we marvel at the stunning feats of resilience and renewal our remarkable planet is capable of. Snowball Earth is science writing at its most gripping and enlightening.
From the Hardcover edition. --This text refers to an alternate kindle_edition edition.
About the Author
GABRIELLE WALKER earned a Ph.D. in natural sciences from Cambridge University. She served as the features editor at New Scientist magazine for seven years and is currently a contributing editor there. She has also taught in the science writing program at Princeton University. Her travels in search of stories have taken her to all seven continents—including a stint at the South Pole.
From the Hardcover edition. --This text refers to an alternate kindle_edition edition.
From the Hardcover edition. --This text refers to an alternate kindle_edition edition.
From Booklist
The Cambrian explosion, which occurred about 600 million years ago when organisms graduated from single-celled monotony to multicelled exuberance, has defied causal explanation. But its coincidence with the ending of an ice age harbors a possible clue. This Precambrian ice era, which froze the entire surface of the earth for 200 million years or more, has, over the past 15 years, become an accepted if startling fact in geological circles, and like many upstart theories in science, its adoption contains stories of research and rivalry. Walker chronicles them through the principals in the debate, focusing mainly on one Paul Hoffman. Walker characterizes him in an unflattering light but presents a positive picture of Hoffman's relentless advocacy of the frozen-earth theory. She also dramatizes with fairness the opponents' alternative interpretations of the main geologic evidence, creating narrative tension that shows science in action. Including vignettes about fieldwork, Walker registers the feel of doing the actual work of geology, especially the thrilling hunt for traces of a frigid apocalypse. Gilbert Taylor
Copyright © American Library Association. All rights reserved --This text refers to an alternate kindle_edition edition.
Copyright © American Library Association. All rights reserved --This text refers to an alternate kindle_edition edition.
Excerpt. © Reprinted by permission. All rights reserved.
ONE
First Fumblings
This is an extraordinary time to be alive. Look around you, take in the intricate complexities of life on Earth, and then consider this: complex life is a very recent invention. Our home planet spent most of its long history coated in nothing but simple, primordial slime. For billions of years, the only earthlings were made of goo.
Then, suddenly, everything changed. At one abrupt moment roughly 600 million years ago, something shook the Earth out of its complacency. From this came the beginnings of eyes, teeth, legs, wings, feathers, hair and brains. Every insect, every ape and antelope, every fish, bird and worm. Whatever triggered this new beginning was ultimately responsible for the existence of you and everyone you've ever known.
So what was it?
Paul Hoffman, part-time marathon runner, full-time geologist, and obsessive, intense seeker of glory, thinks he knows. He believes he has finally struck science gold. Now a full professor at Harvard University and a world-renowned scientist, he has uncovered evidence for the biggest climate catastrophe the Earth has ever endured. And from that disaster, according to Paul, came a remarkable new redemption.
Shark Bay shows up from the air as a snag in the smooth coastline of Western Australia. Five hundred miles north of Perth, it lies just at the place where tropical and temperate zones rub shoulders. The area around the bay is a powerful reminder of how far we have come since primordial slime ruled the world. It is full of varied, vivid life.
This is one of the few places in the world where wild dolphins commune with humans, every day, regular as clockwork. At 7:00 a.m. each day a park ranger dressed in khaki uniform emerges from a wooden hut to focus a pair of binoculars on the horizon. Perhaps half an hour later, he'll spot the first dolphin fin. Somehow the word immediately spreads. Where there were only four or five people on the sandy beach, suddenly fifty or sixty appear.
Three harassed rangers do their best to marshal them into an orderly line. Everyone will get a chance to see the dolphins. No one will be permitted to touch them. No one must go more than knee-deep in the water. Another ranger deftly diverts the enormous wild white pelicans away from the beach by flicking on a water sprinkler. The birds flock around with gaping jaws--in this desert landscape, fresh water is irresistible.
The dolphins and their calves arrive. One of the rangers, a wireless headset amplifying her voice, wades up and down in front of the spectators, introducing the dolphins ("This is Nicky and Nomad, Surprise and her calf Sparky") and reciting useful dolphin facts. The crowd surges into the water, like acolytes seeking a Jordanian baptism, their expressions beatific.
The dolphins are the crowd pullers--more than six hundred of them live here. But Shark Bay is also famous for the rest of its wildlife. The bay contains more than 2,600 tiger sharks, not to mention hammerheads and the occasional great white. The tigers show up in the water as streamlined shadows up to twelve feet long; often they are skulking beside patches of sea grass in the hope that dinner will emerge in the form of a blunt-nosed, lumbering gray dugong. Dugongs, or sea cows, are supposedly the creatures behind the mermaid myths, though I can't see it myself. They are too prosaic, placidly chewing away at the end of a "food trail," a line of clear water that they have cut, caterpillar-like, through the fuzzy green sea grass. They're exceptionally shy and rare, but here, among the largest and richest sea-grass meadows in the world, are a staggering ten thousand of them--tiger sharks notwithstanding.
Then there are sea snakes, green turtles, and migrating humpback whales. And just a little to the north, where the tropics begin in earnest, lies Coral Bay--one of the world's top ten dive sites. Come and dive the Navy pier! See more than 150 species of fish! Also sea sponges and corals, brilliant purple Xatworms, snails and lobsters and shrimp. And the vast, harmless whale sharks, the world's biggest Fish. And on land there are wallabies and bettongs and bandicoots, emus and kangaroos and tiny, timid native mice.
There's everything in this region, from the wonderful to the plain weird. Evolution has been tweaking, adapting and inventing new forms of complex life for hundreds of millions of years, and here in Western Australia it surely shows.
But this is also a place where you can travel back in time, to see the other side of the evolutionary equation--the simplest, most primitive creatures of all. They come from the very First moments in the history of life, just after the dust from the Earth's creation had settled. And when these First fumblings of life appeared on Earth's surface, their form was exceedingly unprepossessing. Throughout oceans, ponds and pools, countless microscopic creatures huddled together in a primordial sludge. They coated the seaXoor, and inched their way up shore with the tide; they clustered around steaming hot springs, and soaked up rays from the faint young sun. Dull green or brown, excreting a gloopy glue that bonded them together into mats, these creatures were little more than bags of soup. Each occupied a single cell. Each had barely mastered the rubrics of how to eat, grow and reproduce. They were like individual cottage industries in a world that had no interest in collaboration or specialization. They were as simple as life gets.
Although these primitive slime creatures have now been outcompeted in all but the most hostile environments, a few odd places still exist where you can experience the primeval Earth firistband. The acidic hot springs of Yellowstone National Park, for instance, or Antarctica's frigid valleys. And here, in Western Australia, where countless microscopic, single-celled, supremely ancient creatures are making their meager living in one small corner of Shark Bay: a shallow lagoon called Hamelin Pool. The pool's water doesn't mix much with the rest of the bay, and it's twice as salty as normal. Since few modern marine animals will tolerate so much salt, this is one of the last refuges of ancient slime.
The sign pointing to Hamelin Pool is easy to miss, even on the desolate road running south from Monkey Mia. On the second pass I Finally spot it, turn left, and bump along a sand track with scrubby bush to either side. For this first visit I avoid the restored telegraph station with its tiny museum and tea shop, and head straight for the beach. I want to experience primordial Earth without a guide.
There's an empty parking lot of white sand, with wattles and low-slung saltbushes clinging to the surrounding dunes, and a path threading through the bushes toward the sea. Though I've come to find the world's simplest creatures, the complexities of life are everywhere. From one of the bushes a chiming wedgebill incessantly reiterates its five-note melody. From another, a gray-crested pigeon regards me unblinkingly. The shells of the beach crunch underfoot; they are tiny, bone-white, and perfectly formed, and the bivalves that grew them are eons of evolution ahead of the simple creatures that I'm seeking. I step onto the boardwalk, which stretches like a pier out into the water. Each weathered plank of wood contains row upon row of cells that once collaborated in a large, complex organism. Signs on all sides show pictures of the slime creatures with smily faces and cheery explanations of their origin. Flies buzz infuriatingly around my head, landing on my face to drink from the corners of my eyes. Black swifts swoop between the handrails, and butterXies the color of honey, with white and black tips to their wings. Time travel is harder than it looks. The modern world is right here even in Hamelin Pool, and it's stubbornly refusing to leave.
I retreat to the telegraph station to plead with the ranger for permission to leave the boardwalk and wade out into the pool. He hesitates and then relents. "Go along the beach to the left," he says. "Don't step on the mats. Be careful." The mats he's talking about are one of the signs of primeval Earth. They are slimy conglomerates of ancient cyanobacteria, and they grow painfully slowly. At the beginning of the last century, horse-drawn wagons were backed into the sea over the mats, to unload boat cargo. A hundred years later the tracks they left are still visible as bare patches in the thin black sludge. An injudicious footprint here will last a long time. I promise to watch my step.
I return to the beach and this time walk carefully toward the water's edge. More striking than the ubiquitous patches of sludgy, foul-smelling bacterial mats are the "living rocks" in between. These strange denizens of Slimeworld are everywhere, an army of misshapen black cabbage heads marching into the sea.
The ones highest up the shore are now nothing more than dead gray domes of rock, shaped like clubs, perhaps a foot tall. They once bore microbial mats on their surfaces, but these have long since shriveled, abandoned by the receding water. Closer to the Pool's edge the domes are coated with black stippling that will turn to dull olive green when the tide washes over them. Most of the stromatolites, though, lie in the water, stretching out as far as I can see. Between them the sand is draped with black-green mats of slime, and checkered with irregular patterns of sunlight as the waves ripple overhead. I wade up to my knees among these strange formations, basking in the sunshine. There is nobody else in sight.
The living rocks of Slimeworld are called "stromatolites," a word that comes from the Greek meaning "bed of rock." Though the interior of the stromatolites is plain, hard rock, their outer layers are spongy to the touch. Here on the surface is where the ancient microbes live. They're sun-worshipers: by day they draw themselves up to their full Wlamentous height--perhaps a thousandth of an inch--soak up the sun, and make their food; by night they lie back down again. The water that surrounds them is Wlled with Wne sand and sediment stirred up by the waves. Gradually this sand rains down on the organisms, and each night's bed is a fresh layer of incipient rock. The stromatolites are inadvertent building sites; the sticky ooze that the organisms extrude acts as mortar and the sand acts as bricks. Every day, as the microbes worm their way outward, another thin layer of rock is laid down beneath them.
It's a slow process. Stromatolites grow just a fraction of an inch each year. The ones in Hamelin Pool are hundreds of years old and would be astonishing feats of engineering, had they been created by design. For these microorganisms to erect a stromatolite three feet high is like humans building something that reaches hundreds of miles into the sky, and scrapes the edges of space. I wade a hundred yards, two hundred yards oVshore, and the slope is still so gentle that the deepening is barely perceptible. Mercifully, the Xies and butterXies have dropped back, and the birdsong is out of earshot. At last I begin to feel that I've traveled back to life's earliest days.
Hamelin Pool's mats and stromatolites look utterly alien, but they were once ubiquitous. Time was, this scene of stromatolites and stippled microbial mats would have greeted you everywhere you went. Forget dolphins and wallabies. This is how the Earth looked for nearly three and a half billion years. The imprints of the stromatolites and their mats show up still wherever suYciently ancient rocks poke through to the Earth's surface. I've seen them in Namibia, in South Africa, in Australia and California. They are sometimes dome-shaped like these in Shark Bay, sometimes cones, sometimes branching like corals. There are places where you can walk among ancient petrified stromatolite reefs, rest your feet on their stone cabbage heads, and see where they have been sliced through to reveal rings of petrified growth. And you can run your Wingers over fossilized mats, which give rock surfaces the unexpected texture of elephant skin. This slime used to be everywhere, and now it's almost nowhere.
How did we get from there to here? This is at once a simpler and more powerful question than it seems. Of course, life took many separate evolutionary steps on its way from stromatolites to wallabies. It had to invent eyes and legs and fur and feet, and everything else that distinguishes marsupials from slime. But there was one particular step that was more important than all the others, one that made all the divergence.
The step was this: learning to make an organism not from just one cell, but from many. Though the first microbes on Earth were woefully unsophisticated, they did gradually learn new tricks to exploit the planet's many niches. But they all still had one thing in common. Each individual creature was packaged in its own tiny sac, a single microscopic cell. Then at some particular point in Earth's history, everything changed. One cell split into two, then four. From that time onward, organisms could be cooperative, and above all their cells could specialize. There could be eye cells and skin cells, cells to make up organs and tissues and limbs.
For life, this was the industrial revolution. Forget the old cottage industries. Now you could have factories with production lines. Parceling out tasks and specializing is always more efficient than trying to do everything yourself. And there are some things, wallabies for instance, that can only be made with a massive collaborative effortt.
In just the same way, when organisms developed the ability to become multicellular, they gained a world of possibilities. Your body is made up of trillions of cells. Every hair is packed with them. You shed skin cells whenever you move. Your blood cells carry energy around your body, to feed the organs made up of still more cells. This multiple identity is the one criterion that's vital for any complex creation. Every dolphin and dugong, every shark, pelican and wombat depends for its existence on that crucial leap from one cell to many. This was the point when simple slime yielded its preeminence to the complex creations that heaved their way out of the sludge and started their march toward modernity.
But why did it take so long? The Slimeworld lasted for almost the whole of Earth history. Let's put in some numbers. Our planet had been around for 4 billion years before the First complex earthlings emerged from the ooze. That's nearly 90 percent of Earth's lifetime.
Four billion years is an insane amount of time, almost impossible to contemplate. There have been many attempts to capture this spread of time in ways that we can comprehend. If the history of life on Earth were crammed into a year, slime would have ruled through spring, summer and fall, continuing well past Halloween into the beginnings of winter. If it were squeezed into the six days of creation, slime ruled until six o'clock on Saturday morning. If it stretched over a marathon course, slime would have led the Weld past the twenty-three-mile mark.
From the Hardcover edition. --This text refers to an alternate kindle_edition edition.
First Fumblings
This is an extraordinary time to be alive. Look around you, take in the intricate complexities of life on Earth, and then consider this: complex life is a very recent invention. Our home planet spent most of its long history coated in nothing but simple, primordial slime. For billions of years, the only earthlings were made of goo.
Then, suddenly, everything changed. At one abrupt moment roughly 600 million years ago, something shook the Earth out of its complacency. From this came the beginnings of eyes, teeth, legs, wings, feathers, hair and brains. Every insect, every ape and antelope, every fish, bird and worm. Whatever triggered this new beginning was ultimately responsible for the existence of you and everyone you've ever known.
So what was it?
Paul Hoffman, part-time marathon runner, full-time geologist, and obsessive, intense seeker of glory, thinks he knows. He believes he has finally struck science gold. Now a full professor at Harvard University and a world-renowned scientist, he has uncovered evidence for the biggest climate catastrophe the Earth has ever endured. And from that disaster, according to Paul, came a remarkable new redemption.
Shark Bay shows up from the air as a snag in the smooth coastline of Western Australia. Five hundred miles north of Perth, it lies just at the place where tropical and temperate zones rub shoulders. The area around the bay is a powerful reminder of how far we have come since primordial slime ruled the world. It is full of varied, vivid life.
This is one of the few places in the world where wild dolphins commune with humans, every day, regular as clockwork. At 7:00 a.m. each day a park ranger dressed in khaki uniform emerges from a wooden hut to focus a pair of binoculars on the horizon. Perhaps half an hour later, he'll spot the first dolphin fin. Somehow the word immediately spreads. Where there were only four or five people on the sandy beach, suddenly fifty or sixty appear.
Three harassed rangers do their best to marshal them into an orderly line. Everyone will get a chance to see the dolphins. No one will be permitted to touch them. No one must go more than knee-deep in the water. Another ranger deftly diverts the enormous wild white pelicans away from the beach by flicking on a water sprinkler. The birds flock around with gaping jaws--in this desert landscape, fresh water is irresistible.
The dolphins and their calves arrive. One of the rangers, a wireless headset amplifying her voice, wades up and down in front of the spectators, introducing the dolphins ("This is Nicky and Nomad, Surprise and her calf Sparky") and reciting useful dolphin facts. The crowd surges into the water, like acolytes seeking a Jordanian baptism, their expressions beatific.
The dolphins are the crowd pullers--more than six hundred of them live here. But Shark Bay is also famous for the rest of its wildlife. The bay contains more than 2,600 tiger sharks, not to mention hammerheads and the occasional great white. The tigers show up in the water as streamlined shadows up to twelve feet long; often they are skulking beside patches of sea grass in the hope that dinner will emerge in the form of a blunt-nosed, lumbering gray dugong. Dugongs, or sea cows, are supposedly the creatures behind the mermaid myths, though I can't see it myself. They are too prosaic, placidly chewing away at the end of a "food trail," a line of clear water that they have cut, caterpillar-like, through the fuzzy green sea grass. They're exceptionally shy and rare, but here, among the largest and richest sea-grass meadows in the world, are a staggering ten thousand of them--tiger sharks notwithstanding.
Then there are sea snakes, green turtles, and migrating humpback whales. And just a little to the north, where the tropics begin in earnest, lies Coral Bay--one of the world's top ten dive sites. Come and dive the Navy pier! See more than 150 species of fish! Also sea sponges and corals, brilliant purple Xatworms, snails and lobsters and shrimp. And the vast, harmless whale sharks, the world's biggest Fish. And on land there are wallabies and bettongs and bandicoots, emus and kangaroos and tiny, timid native mice.
There's everything in this region, from the wonderful to the plain weird. Evolution has been tweaking, adapting and inventing new forms of complex life for hundreds of millions of years, and here in Western Australia it surely shows.
But this is also a place where you can travel back in time, to see the other side of the evolutionary equation--the simplest, most primitive creatures of all. They come from the very First moments in the history of life, just after the dust from the Earth's creation had settled. And when these First fumblings of life appeared on Earth's surface, their form was exceedingly unprepossessing. Throughout oceans, ponds and pools, countless microscopic creatures huddled together in a primordial sludge. They coated the seaXoor, and inched their way up shore with the tide; they clustered around steaming hot springs, and soaked up rays from the faint young sun. Dull green or brown, excreting a gloopy glue that bonded them together into mats, these creatures were little more than bags of soup. Each occupied a single cell. Each had barely mastered the rubrics of how to eat, grow and reproduce. They were like individual cottage industries in a world that had no interest in collaboration or specialization. They were as simple as life gets.
Although these primitive slime creatures have now been outcompeted in all but the most hostile environments, a few odd places still exist where you can experience the primeval Earth firistband. The acidic hot springs of Yellowstone National Park, for instance, or Antarctica's frigid valleys. And here, in Western Australia, where countless microscopic, single-celled, supremely ancient creatures are making their meager living in one small corner of Shark Bay: a shallow lagoon called Hamelin Pool. The pool's water doesn't mix much with the rest of the bay, and it's twice as salty as normal. Since few modern marine animals will tolerate so much salt, this is one of the last refuges of ancient slime.
The sign pointing to Hamelin Pool is easy to miss, even on the desolate road running south from Monkey Mia. On the second pass I Finally spot it, turn left, and bump along a sand track with scrubby bush to either side. For this first visit I avoid the restored telegraph station with its tiny museum and tea shop, and head straight for the beach. I want to experience primordial Earth without a guide.
There's an empty parking lot of white sand, with wattles and low-slung saltbushes clinging to the surrounding dunes, and a path threading through the bushes toward the sea. Though I've come to find the world's simplest creatures, the complexities of life are everywhere. From one of the bushes a chiming wedgebill incessantly reiterates its five-note melody. From another, a gray-crested pigeon regards me unblinkingly. The shells of the beach crunch underfoot; they are tiny, bone-white, and perfectly formed, and the bivalves that grew them are eons of evolution ahead of the simple creatures that I'm seeking. I step onto the boardwalk, which stretches like a pier out into the water. Each weathered plank of wood contains row upon row of cells that once collaborated in a large, complex organism. Signs on all sides show pictures of the slime creatures with smily faces and cheery explanations of their origin. Flies buzz infuriatingly around my head, landing on my face to drink from the corners of my eyes. Black swifts swoop between the handrails, and butterXies the color of honey, with white and black tips to their wings. Time travel is harder than it looks. The modern world is right here even in Hamelin Pool, and it's stubbornly refusing to leave.
I retreat to the telegraph station to plead with the ranger for permission to leave the boardwalk and wade out into the pool. He hesitates and then relents. "Go along the beach to the left," he says. "Don't step on the mats. Be careful." The mats he's talking about are one of the signs of primeval Earth. They are slimy conglomerates of ancient cyanobacteria, and they grow painfully slowly. At the beginning of the last century, horse-drawn wagons were backed into the sea over the mats, to unload boat cargo. A hundred years later the tracks they left are still visible as bare patches in the thin black sludge. An injudicious footprint here will last a long time. I promise to watch my step.
I return to the beach and this time walk carefully toward the water's edge. More striking than the ubiquitous patches of sludgy, foul-smelling bacterial mats are the "living rocks" in between. These strange denizens of Slimeworld are everywhere, an army of misshapen black cabbage heads marching into the sea.
The ones highest up the shore are now nothing more than dead gray domes of rock, shaped like clubs, perhaps a foot tall. They once bore microbial mats on their surfaces, but these have long since shriveled, abandoned by the receding water. Closer to the Pool's edge the domes are coated with black stippling that will turn to dull olive green when the tide washes over them. Most of the stromatolites, though, lie in the water, stretching out as far as I can see. Between them the sand is draped with black-green mats of slime, and checkered with irregular patterns of sunlight as the waves ripple overhead. I wade up to my knees among these strange formations, basking in the sunshine. There is nobody else in sight.
The living rocks of Slimeworld are called "stromatolites," a word that comes from the Greek meaning "bed of rock." Though the interior of the stromatolites is plain, hard rock, their outer layers are spongy to the touch. Here on the surface is where the ancient microbes live. They're sun-worshipers: by day they draw themselves up to their full Wlamentous height--perhaps a thousandth of an inch--soak up the sun, and make their food; by night they lie back down again. The water that surrounds them is Wlled with Wne sand and sediment stirred up by the waves. Gradually this sand rains down on the organisms, and each night's bed is a fresh layer of incipient rock. The stromatolites are inadvertent building sites; the sticky ooze that the organisms extrude acts as mortar and the sand acts as bricks. Every day, as the microbes worm their way outward, another thin layer of rock is laid down beneath them.
It's a slow process. Stromatolites grow just a fraction of an inch each year. The ones in Hamelin Pool are hundreds of years old and would be astonishing feats of engineering, had they been created by design. For these microorganisms to erect a stromatolite three feet high is like humans building something that reaches hundreds of miles into the sky, and scrapes the edges of space. I wade a hundred yards, two hundred yards oVshore, and the slope is still so gentle that the deepening is barely perceptible. Mercifully, the Xies and butterXies have dropped back, and the birdsong is out of earshot. At last I begin to feel that I've traveled back to life's earliest days.
Hamelin Pool's mats and stromatolites look utterly alien, but they were once ubiquitous. Time was, this scene of stromatolites and stippled microbial mats would have greeted you everywhere you went. Forget dolphins and wallabies. This is how the Earth looked for nearly three and a half billion years. The imprints of the stromatolites and their mats show up still wherever suYciently ancient rocks poke through to the Earth's surface. I've seen them in Namibia, in South Africa, in Australia and California. They are sometimes dome-shaped like these in Shark Bay, sometimes cones, sometimes branching like corals. There are places where you can walk among ancient petrified stromatolite reefs, rest your feet on their stone cabbage heads, and see where they have been sliced through to reveal rings of petrified growth. And you can run your Wingers over fossilized mats, which give rock surfaces the unexpected texture of elephant skin. This slime used to be everywhere, and now it's almost nowhere.
How did we get from there to here? This is at once a simpler and more powerful question than it seems. Of course, life took many separate evolutionary steps on its way from stromatolites to wallabies. It had to invent eyes and legs and fur and feet, and everything else that distinguishes marsupials from slime. But there was one particular step that was more important than all the others, one that made all the divergence.
The step was this: learning to make an organism not from just one cell, but from many. Though the first microbes on Earth were woefully unsophisticated, they did gradually learn new tricks to exploit the planet's many niches. But they all still had one thing in common. Each individual creature was packaged in its own tiny sac, a single microscopic cell. Then at some particular point in Earth's history, everything changed. One cell split into two, then four. From that time onward, organisms could be cooperative, and above all their cells could specialize. There could be eye cells and skin cells, cells to make up organs and tissues and limbs.
For life, this was the industrial revolution. Forget the old cottage industries. Now you could have factories with production lines. Parceling out tasks and specializing is always more efficient than trying to do everything yourself. And there are some things, wallabies for instance, that can only be made with a massive collaborative effortt.
In just the same way, when organisms developed the ability to become multicellular, they gained a world of possibilities. Your body is made up of trillions of cells. Every hair is packed with them. You shed skin cells whenever you move. Your blood cells carry energy around your body, to feed the organs made up of still more cells. This multiple identity is the one criterion that's vital for any complex creation. Every dolphin and dugong, every shark, pelican and wombat depends for its existence on that crucial leap from one cell to many. This was the point when simple slime yielded its preeminence to the complex creations that heaved their way out of the sludge and started their march toward modernity.
But why did it take so long? The Slimeworld lasted for almost the whole of Earth history. Let's put in some numbers. Our planet had been around for 4 billion years before the First complex earthlings emerged from the ooze. That's nearly 90 percent of Earth's lifetime.
Four billion years is an insane amount of time, almost impossible to contemplate. There have been many attempts to capture this spread of time in ways that we can comprehend. If the history of life on Earth were crammed into a year, slime would have ruled through spring, summer and fall, continuing well past Halloween into the beginnings of winter. If it were squeezed into the six days of creation, slime ruled until six o'clock on Saturday morning. If it stretched over a marathon course, slime would have led the Weld past the twenty-three-mile mark.
From the Hardcover edition. --This text refers to an alternate kindle_edition edition.
Product details
- ASIN : B000XUDG8K
- Publisher : Crown (December 18, 2007)
- Publication date : December 18, 2007
- Language : English
- File size : 560 KB
- Text-to-Speech : Enabled
- Screen Reader : Supported
- Enhanced typesetting : Enabled
- X-Ray : Not Enabled
- Word Wise : Enabled
- Print length : 288 pages
- Lending : Not Enabled
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- #433 in Geography (Kindle Store)
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Reviewed in the United States on August 2, 2017
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The theory is developed by the author through a sequence of contributors spanning 60 years. The geology is at a level that a novice could understand. I would have preferred more information about isotopic analysis and paleomagnetism. Photos would have been nice as well showing the clear boundary between drop stone deposits and the overlying carbonates. The description of sandstone wedges is another missed photo opportunity. Like John McPhee, the author uses the personalities of the contributors to enhance the tale. Lastly, I very much enjoyed the detailed look at deposits just prior (in geologic terms) before the Cambrian Explosion. The closing of the Pre-Cambrian matches the closing of the Paleozoic and Mesozoic Eras for "excitement" on a global scale. So much for Uniformitarianism!
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Reviewed in the United States on October 3, 2019
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the story of how a succession of scientists untangled complex clues to discover and document the processes whereby Earth became entirely covered with ice (as many as 5 times!), and how the planet was saved by emissions of carbon dioxide from Volcanos (which did not undergo the normal absorbtion into rocks and ocean because both were covered by the ice); and how other, disbelieving scientists disparaged and sought to debunk Snowballism
the book also examines whether this could happen again, and when
the author (with a PhD from Cambridge in natural sciences) didn't merely interview the many scientists involved, but also traveled with them on expeditions to their farflung field sites to find and examine the evidentiary rocks and fossils and other clues to Earth's early history
the book also examines whether this could happen again, and when
the author (with a PhD from Cambridge in natural sciences) didn't merely interview the many scientists involved, but also traveled with them on expeditions to their farflung field sites to find and examine the evidentiary rocks and fossils and other clues to Earth's early history
Reviewed in the United States on May 9, 2003
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It is fascinating to watch the unfolding of new scientific theories, particularly after having lived through some of them. For example, when I first began studying geology, continental drift was just beginning to be accepted. This book advances some interesting ideas in Earth history that seem to have good evidence for them. It's also well written and entertaining (although, I agree with the other reviewer who called it too "dumbed down").
The book really, really needs illustrations (there are NONE), and it's astonishing that it does not have them, given the opportunities. There are the stunning landscapes of Namibia and Svalbard that could appear. There really should be photos of the Hamelin Pool, of Stromatolite fossils, of the minerals and rock formations, and of the geologist protagonists. I'd recommend fifty color photos, and I will buy another copy if a new edition is produced that way.
Minor gripe: There's only one place in the world one can have an "intercontinental train" -- and it's not Canada. Proofreader, hello?
All in all, a very worthwhile read.
For those who may wish to study the matter further, there is a "snowballearth.org" with a lot of bibliography, photos, etc. Increasing interest in Precambrian glaciation has resulted in many new scientific papers in the last few years.
The book really, really needs illustrations (there are NONE), and it's astonishing that it does not have them, given the opportunities. There are the stunning landscapes of Namibia and Svalbard that could appear. There really should be photos of the Hamelin Pool, of Stromatolite fossils, of the minerals and rock formations, and of the geologist protagonists. I'd recommend fifty color photos, and I will buy another copy if a new edition is produced that way.
Minor gripe: There's only one place in the world one can have an "intercontinental train" -- and it's not Canada. Proofreader, hello?
All in all, a very worthwhile read.
For those who may wish to study the matter further, there is a "snowballearth.org" with a lot of bibliography, photos, etc. Increasing interest in Precambrian glaciation has resulted in many new scientific papers in the last few years.
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Reviewed in the United States on April 28, 2005
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Who among us is not interested in the history of our own blue-white planet and the origin of life, even if it is only through creation myths?
Author, Gabrielle Walker earned her Ph.D. in chemistry at Cambridge University and spent seven years as a features editor at "New Scientist." The latter experience definitely had a hand in molding her breezy, yet clear and conscientious style. She follows her intrepid geologists to the ends of the Earth like an eager cub reporter in some 1930s B-movie, peppering them with questions, almost getting trampled by an African elephant in the Namibian bush, beset by freezing fog in the Kalahari Desert, clambering down the windswept, godforsaken rocks of Mistaken Point in Newfoundland.
This book is a combination travel guide to some of the least habitable places on earth, biographical sketches of the scientists who developed and tested the 'Snowball Earth' theory, and an introduction to the painstaking science behind the newest, most audacious 'deep time' history of our planet.
Before we get to 'Snowball Earth,' let me give you a flavor of Walker's running travelogue. Here she is speaking of Mistaken Point: "Nobody could love these barren lands, not even their mother. They are dreary and damp, their plants the color of overcooked spinach and rusty nails; when the wind is not buffeting them or rain beating them down, they are shrouded in fog. The pale, thin caribou wander over them like lost souls."
Now, on to the theory as expounded by this book. Several times in the history of Earth, most recently 700 million years ago, our planet froze completely over, possibly because all of the continents had migrated close to the Equator. This deep-freeze may have ended the multi-billion-year reign of single-cell slime and given a kick-start to the Cambrian explosion of complex life. Snowball Earth was finally melted by a build-up of carbon dioxide in the atmosphere, courtesy of volcanic eruptions which turned our planet into a hellish, hurricane-ripped green-house. Eventually the excess carbon dioxide was absorbed back into the oceans and the planetary crust. Multi-cellular life reveled in the first decent climate it had ever experienced, not realizing that meteor strikes and volcanic eruptions would occasionally wipe out up to 90% of its evolved species.
Could we get a repeat of Snowball Earth? Sure. As a matter of fact, the continents seem to be sliding toward the Equator again, which will allow ice to build up at the Poles and advance toward Earth's bulging midline. Will this happen during our lifetime? Nah. As Gabrielle Walker so vividly expresses it, the continental plates move at roughly the same speed our fingernails grow.
The geologists, paleontologists, and their science form the core of this marvelously written book. Walker does a meticulous job of relating both the scientific and the human side of the 'Snowball Earth' controversy. Her incisive portraits of the scientific movers and shakers, most especially the fiercely competitive Paul Hoffman, will stick in your mind long after you forget about drop stones, tidal rhythmites, and magnetic reversals in the Flinders ice rocks.
Author, Gabrielle Walker earned her Ph.D. in chemistry at Cambridge University and spent seven years as a features editor at "New Scientist." The latter experience definitely had a hand in molding her breezy, yet clear and conscientious style. She follows her intrepid geologists to the ends of the Earth like an eager cub reporter in some 1930s B-movie, peppering them with questions, almost getting trampled by an African elephant in the Namibian bush, beset by freezing fog in the Kalahari Desert, clambering down the windswept, godforsaken rocks of Mistaken Point in Newfoundland.
This book is a combination travel guide to some of the least habitable places on earth, biographical sketches of the scientists who developed and tested the 'Snowball Earth' theory, and an introduction to the painstaking science behind the newest, most audacious 'deep time' history of our planet.
Before we get to 'Snowball Earth,' let me give you a flavor of Walker's running travelogue. Here she is speaking of Mistaken Point: "Nobody could love these barren lands, not even their mother. They are dreary and damp, their plants the color of overcooked spinach and rusty nails; when the wind is not buffeting them or rain beating them down, they are shrouded in fog. The pale, thin caribou wander over them like lost souls."
Now, on to the theory as expounded by this book. Several times in the history of Earth, most recently 700 million years ago, our planet froze completely over, possibly because all of the continents had migrated close to the Equator. This deep-freeze may have ended the multi-billion-year reign of single-cell slime and given a kick-start to the Cambrian explosion of complex life. Snowball Earth was finally melted by a build-up of carbon dioxide in the atmosphere, courtesy of volcanic eruptions which turned our planet into a hellish, hurricane-ripped green-house. Eventually the excess carbon dioxide was absorbed back into the oceans and the planetary crust. Multi-cellular life reveled in the first decent climate it had ever experienced, not realizing that meteor strikes and volcanic eruptions would occasionally wipe out up to 90% of its evolved species.
Could we get a repeat of Snowball Earth? Sure. As a matter of fact, the continents seem to be sliding toward the Equator again, which will allow ice to build up at the Poles and advance toward Earth's bulging midline. Will this happen during our lifetime? Nah. As Gabrielle Walker so vividly expresses it, the continental plates move at roughly the same speed our fingernails grow.
The geologists, paleontologists, and their science form the core of this marvelously written book. Walker does a meticulous job of relating both the scientific and the human side of the 'Snowball Earth' controversy. Her incisive portraits of the scientific movers and shakers, most especially the fiercely competitive Paul Hoffman, will stick in your mind long after you forget about drop stones, tidal rhythmites, and magnetic reversals in the Flinders ice rocks.
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John Southern
5.0 out of 5 stars
A very plausible theory
Reviewed in the United Kingdom on April 5, 2012Verified Purchase
One would need no previous knowledge of geology to enjoy this book. It is as much about the scientific community as it is about the science. The proposal that perhaps more than once life came to a total standstill on earth seems far fetched. But the evidence is there and it will be for future geologists to find other explanations for the evidence if they can. I learnt from this narrative that this is how "truth" is established in all sciences.
Amazon Customer
4.0 out of 5 stars
SNOW BALL
Reviewed in the United Kingdom on February 24, 2019Verified Purchase
INTERESTING BOOK
