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Extinction: How Life on Earth Nearly Ended 250 Million Years Ago [Hardcover]

Douglas H. Erwin (Author)
4.1 out of 5 stars  See all reviews (19 customer reviews)


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Book Description

0691005249 978-0691005249 January 30, 2006

Some 250 million years ago, the earth suffered the greatest biological crisis in its history. Around 95% of all living species died out--a global catastrophe far greater than the dinosaurs' demise 65 million years ago. How this happened remains a mystery. But there are many competing theories. Some blame huge volcanic eruptions that covered an area as large as the continental United States; others argue for sudden changes in ocean levels and chemistry, including burps of methane gas; and still others cite the impact of an extraterrestrial object, similar to what caused the dinosaurs' extinction.

Extinction is a paleontological mystery story. Here, the world's foremost authority on the subject provides a fascinating overview of the evidence for and against a whole host of hypotheses concerning this cataclysmic event that unfolded at the end of the Permian.

After setting the scene, Erwin introduces the suite of possible perpetrators and the types of evidence paleontologists seek. He then unveils the actual evidence--moving from China, where much of the best evidence is found; to a look at extinction in the oceans; to the extraordinary fossil animals of the Karoo Desert of South Africa. Erwin reviews the evidence for each of the hypotheses before presenting his own view of what happened.

Although full recovery took tens of millions of years, this most massive of mass extinctions was a powerful creative force, setting the stage for the development of the world as we know it today.



Editorial Reviews

Review

Theories and mysteries can be dispelled with good data from the geologic record, and Erwin (a paleobiologist at the Smithsonian Institution's National Museum of Natural History) offers an authoritative account of the search for these data and for the cause of the extinction. . . . Extinction provides a great reference for researchers and the interested lay reader alike. -- Andrew M. Bush, Science

Extinction is a very enjoyable read. . . . It provides a thoroughly up-to-date account of the causes of the end-Permian event and the developments in the field since 1993 as seen through the eyes of one of the key players. . . . Extinction leaves the reader with the (accurate) picture that here is a scientist whose work has significantly advanced our understanding of the greatest extinction event known to science. . . . [A] readable and scholarly account. -- Richard J. Twitchett, American Scientist

Douglas Erwin's geological mystery story is engrossing. It contains a tribute to the scientific method--and also the collaborations of research. The book ends with Erwin warning that the Earth is arguably entering another mass extinction period, this time unnatural and man-made. And this time the destruction may well be total. -- Lucy Sussex, The Age

Douglas Erwin describes how life on Earth was nearly destroyed at the end of the Permian period, 250 million years ago. . . . The author . . . explain[s] what this paleontological, as well as geological, evidence can tell scientists about the dramatic and deadly shift in the Earth's environment. -- Science News

Douglas H. Erwin, a Smithsonian paleobiologist and one of the leading experts on the Permian extinction has meticulously sifted through the evidence. . . . His accessible new book, Extinction--written, it seems, both to persuade his colleagues and to educate a lay audience--is told from the perspective of a forensic scientist trying to piece together a quarter-billion-year-old crime scene. -- Joshua Foer, Washington Post Book World

No one can tell this story better than Douglas Erwin. His book is a superbly written account of what we know about the Permian extinctions. . . . More than a geological story, this book is an excellent model of how science addresses complicated questions. -- Choice

This book does not justify a single, accepted causal sequence of events . . . to account for the end-Permian extinction. Instead, Erwin dissects the evidence for and against each hypothesis, impartially weighing their strengths and weaknesses. Although this book may frustrate readers expecting to learn how life nearly ended 250 million years ago, it will reward them with a fascinating case study in scientific inference, a case that remains very much open. -- John P. Hunter, Quarterly Review of Biology

Erwin's book is science writing for the general public at its best and most lucid. Entertaining, informative, and thought provoking. -- Northeastern Naturalist

Erwin offers a thorough overview of one of the most interesting problems in earth history. . . . Erwin takes the readers on an insider's journey that includes adventures in the field, tedious hours in the laboratory, and stimulating but sometimes contentious exchanges among colleagues at scientific meetings. He gives rigorous consideration to every reasonable hypothesis. . . . Erwin's short course is a professional service for geologists (like me) who have read only some of the primary literature on the end-Permian extinction. -- Stephen O. Moshier, Books & Culture

For scientists as well as general educated readers, this book enlightens its readers to the complexity of the largest biological crisis the earth has yet seen. -- H.J.M. Meijer, PalArch's Journal of Vertebrate Paleontology

I recommend Extinction: How Life on Earth Nearly Ended 250 Million Years Ago to scientists and nonscientists alike. It provides a clear, comprehensive, and compelling introduction to the greatest catastrophe in the history of animal life and proposes a reasonable hypothesis for the cause of the extinction that will undoubtedly be tested vigorously with new data in the coming decade. -- Jonathan L. Payne, Complexity

From the Inside Flap

"Douglas Erwin blends careful scholarship and graceful prose in this authoritative elucidation of Earth's greatest mass extinction. Although framed in terms of hypotheses and their tests, Erwin's story unfolds as a gripping who-done-it for the ages."--Andrew H. Knoll, Harvard University, author of Life on a Young Planet

"Douglas Erwin is the world's leading expert on the end-Permian extinction. This book will be the standard reference on this crucial event in the history of life. It is a wonderful example of science in action."--Richard Bambach, Virginia Tech

"This book provides an up-to-date review and critical appraisal of all we know about the end-Permian mass extinction, a subject that has drawn much popular attention. Complementing its solid scholarship, its friendly style enables educated general readers to get to grips with all the current debates."--Paul Wignall, University of Leeds, author of Mass Extinctions and Their Aftermaths

"In conversational prose, Douglas Erwin provides a useful roadmap to a complex scientific subject--an up-to-date treatment of the end-Permian extinction."--Michael J. Foote, University of Chicago


Product Details

  • Hardcover: 320 pages
  • Publisher: Princeton University Press (January 30, 2006)
  • Language: English
  • ISBN-10: 0691005249
  • ISBN-13: 978-0691005249
  • Product Dimensions: 9.2 x 6.3 x 1.2 inches
  • Shipping Weight: 1.2 pounds
  • Average Customer Review: 4.1 out of 5 stars  See all reviews (19 customer reviews)
  • Amazon Best Sellers Rank: #320,670 in Books (See Top 100 in Books)

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43 of 44 people found the following review helpful:
5.0 out of 5 stars Splendid agnosticism, November 22, 2006
This review is from: Extinction: How Life on Earth Nearly Ended 250 Million Years Ago (Hardcover)
In Kentucky, there's a museum with a lifesize model of a dinosaur with a saddle on it. This is a hymn in fiberglass to young Earth creationism, the idea that the Universe was created about 6,000 years ago.
It costs $1,500 to become a charter member (family rate) of this museum. A much better investment would be $24.95 for Douglas Erwin's thriller about the Permian extinction.
More than nine-tenths of all species died out 251 million years ago. Erwin, a researcher with the Smithsonian Institution's National Museum of Natural History and the Santa Fe Institute, finds the end-Permian "enigma far more compelling than the end of the dinosaurs," a relatively minor event from 65 million years ago.
For an event that Kentuckians think never happened, the end-Permian event left a lot of debris, of which the most interesting is in China. Until 20 years ago, the paleontological record there was unknown to the outside world.
What the evidence is telling us is difficult to say. Erwin says "Extinction" was "frankly written as a mystery story." In this one, the clever detective does not wrap up all the loose ends on the last page.
Instead, we learn that there are at least seven major theories of what might have happened. These range from a big meteorite to gigantic volcanic eruptions in Siberia to a climatic or biological or geological change that drove oxygen out of the oceans.
The first chapters set the stage. Life was very different in the Permian. There were reefs in warm oceans, and they contained corals, but the corals were only distantly related to those of today and they were not as important as crinoids and lampshells, animals that still exist in out-of-the-way places.
On land, flowering plants had not yet evolved, nor mammals, dinosaurs or saddles. In South Africa's Karoo basin, fossils remain of a fabulous, lost fauna.
There were widespread extinctions on land as well as in the sea during the end-Permian event, but it is hard to say whether the land extinction was as complete as in the sea, where 94 percent of species disappeared in a short time. Erwin's team and their Chinese collaborators have found evidence that it all happened in less than 160,000 years -- maybe a lot less.
It is also not proved that the big land extinction exactly coincided with the sea kill, but it seems likely. The land kill was a whopper, too. This was apparently the only time in history when a mass extinction had any real impact on insects.
Whatever the cause, it did set up the modern world. "Mass extinction is a powerful creative force," says Erwin.
Or did it? As they learn more and more of the details, scientists are also learning to question the easy assumptions of more innocent decades.
Evolutionary biologists are vigorously debating whether the animals and plants that dominated the Permian were already being outcompeted by the early forerunners of modern flora and fauna, or whether they would have maintained their control of resources.
Erwin, splendidly agnostic about this and other debates, lays out the questions but leaves the resolution for some other time. Perhaps not too far in the future. He notes that his 1993 book on the Permian extinction already is out of date in many ways.
In fact, after decades researching the extinction itself, he has now concluded that "understanding the recovery from the extinction poses a far greater intellectual challenge."
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27 of 27 people found the following review helpful:
5.0 out of 5 stars Resetting the clock, May 30, 2006
This review is from: Extinction: How Life on Earth Nearly Ended 250 Million Years Ago (Hardcover)
Any scientist who opens [and closes!] a book by saying "We [I] don't know!" is worthy of your attention and respect. Too many others have taken up a theme and defended against all comers. Erwin's examination of the catastrophic close of the Permian Age is complete, admirably researched and exquisitely written. Within its pages, this work examines the various ideas on the massive loss of life 250 million years ago. These days, not to have heard of an meteor's killing off the dinosaurs 65 million years ago suggests you've lived hidden in a cave for a generation. Erwin opens with a brief overview of that event, reminding us that extinctions, particularly "impact events", have loomed large in discussions of the history of life ever since Walter and Luis Alvarez proposed the idea.

It's easy to rattle off the numbers: when the dinosaurs "went West", perhaps 75% of life was also extinguished. When the Permian ended, over 95% of living things disappeared. Erwin asks: "How do we know this? What life forms disappeared? Did they all go at the same time? How long did it take to recover?" Most important, of course, "What killed them off?" Instead of dull statistics, Erwin asks the important questions. Acknowledging that "Triassic rocks are boring", he explains why this is so. Fossils are scarce is the obvious answer, but why they are missing is his quest. With most of his attention focussed on ocean life, he details what causes shifts in benthic populations. The seas rise and fall - for a variety of reasons. Glaciation takes up sea water and leaves continental shelves high and dry. Oceans need to "turn over" an oxygen supply. What is the result of that failing? Carbon, with its various isotopes, passes through life selectively. Tracing that path provides insights into where it's been - and where not. When did the Siberian "traps" form? How much lava spewed from that rift, and what other products did it bring along or destroy? Finally, is there evidence that Earth was pelted by another bolide to provide an easy answer to all those questions? That reply is almost surely negative.

Erwin would like to couch this narrative as a detective story, but it doesn't really work. There are too many victims - unless you count life as one entity. There is also a phalanx of detectives all trying assiduously to solve the case. If you thought there were too many cooks spoiling the broth, wait until you meet this mob. Nearly all of them have an agenda and they have a disturbing tendency to trumpet a single tune. Erwin should have portrayed them as an orchestra, with himself as conductor. Van Kariajan would go emerald with envy. Each investigator supplies a theme, striving for a solo performance. Erwin cautiously assesses the tune, fits it nicely into a grander theme and produces a symphony instead of a cacophony. It's quite a performance. To keep himself from the sin of hubris, he points out his own flaws in a previous effort. The strain wasn't discordant, but the composition needed refinement.

Erwin fastidiously acknowledges his contributors. Jack Sepkowski comes in for deserved accolades, as do Bruce Rubridge, Yugan Jin and many others. Their methods, results and further work - including that incomplete but "promised" - are given a full hearing. Even those whose suggestions are highly suspicious, such as Luann Becker's Bedout "crater" are given a respectful hearing. Nobody's work is chastised or rejected. "We need more investigation" is the running theme of Erwin's account. The reason the ongoing search is important lies in understanding what is happening around us today. Are we, in Dave Sepkowski's words a "Dead Clade Walking"? Or can we glean enough information from the rocks to find the means to succeed through the extinction we seem to be part of - and likely creating? The "95%" means life had to restart the clock after the Permian. There were a few "Lazarus species" that re-emerged after the cataclysm. Will the human species manage to revive itself when so much life around us has been decimated? No more pertinent question confronts us. [stephen a. haines - Ottawa, Canada]
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24 of 25 people found the following review helpful:
5.0 out of 5 stars When Life Almost Didn't Make It, April 7, 2006
This review is from: Extinction: How Life on Earth Nearly Ended 250 Million Years Ago (Hardcover)
Even kids now can tell you about the mass extinction that wiped out the dinosaurs. When I was a kid, the dinosaur extinction was a big mystery, but there has been good evidence, now broadly accepted, that 65 million years ago a meteor as big as a mountain smashed into the Yucatan, turning everything for miles around into ash, wrapping the world in a cloud, and blocking the sunlight that runs all life. Everything all over the world changed, and we mammals got our try at reproductive success. The horrendous extinction that ended the Cretaceous age, however, wasn't the worst our old Earth had seen. 250 million years ago, there was an extinction that ended the Permian and began the Triassic periods (which is also the border between the larger, more general Paleozoic and Mesozoic eras). This Permo-Triassic event extinguished around 95 percent of all living species, and was as close as we have ever come to having all life wiped out. In fact, in the 19th century, geologists thought that life had been wiped out and a separate creation had occurred to start the Triassic. What really happened, and how, are the subjects of _Extinction: How Life on Earth Nearly Ended 250 Million Years Ago_ (Princeton University Press) by Douglas H. Erwin, Senior Scientist and Curator of the Department of Paleobiology at the Smithsonian. He has made the end-Permian mass extinction his research interest for the past twenty years, and has traveled all over the world to the fossil beds and geologic boundary layers remaining from around the time of the catastrophe. Looking back so many millions of years ago is not easy, and the picture is not as clear as that of the dinosaur extinction. Erwin's book, however, is a fine demonstration of how geologists and paleobiologists have come to some admittedly limited understanding of what happened.

There are many factors that have been suspects in the great killing, and Erwin likes to think of himself as a detective out of Agatha Christie set to finger the actual culprit. It's not that easy, of course. Catastrophic explanations for the end-Permian abound, and Erwin's book is an examination of the more likely causes, about six of them. Of course, a main one, borrowing from the success of the impact explanation of 65 million years ago, is an extraterrestrial impact. It is certainly a plausible explanation, since it is accepted as the cause of the more recent extinction. There are problems, however. The impact that wiped out the dinosaurs left clues like an iridium layer in geological strata (there is lots of iridium in meteorites, not so much on Earth) and "shocked quartz" impact crystals, but such clues are lacking for the earlier event. Another explanation might be volcanism, resulting in dust and acidic chemicals and basalts that cover a countryside "much as honey fills in the roughness of an English muffin." Yet another is that continental drift (plate tectonics) was causing collisions at the time, forcing species that had not previously met each other to compete, and changing the global climate by newly formed landmasses. Vast glaciation may have caused cooling and a decrease in sea level. Perhaps there was a drop in oxygen levels of the oceans. Maybe sea levels dropped and caused a huge release of methane from sediments.

He has not, however, wrapped everything up, as, say, Hercule Poirot might. He does, indeed, call his own proposal at explanation the _Murder on the Orient Express_ hypothesis, based on Agatha Christie's book which is a who-didn't-do-it rather than a whodunit. The explanation calls on aspects of many of the other explanations, but Erwin admits this makes it hard to test. One of his colleagues had dubbed it "Erwin's kitchen sink hypothesis", and, as Erwin says, was not being complimentary. There are implications for our own times in this story, since we are now in another period of great extinctions and our climate may be changing irrevocably, but Erwin does not stress these. His book is a fine summary of current thinking on the extinction. Readers will come up against sentences like, "Some surviving ammonoids with extreme morphology died out in the Griesbachian, but new Dienerian ammonoids were more similar to the norm..." (all the terms are well explained, but will be new to most readers), but then a few pages later readers will learn that the "quality of many Early Triassic fossils is really pretty lousy." There may be fewer hard answers here than in a murder mystery, but the explanations about how scientists came up with ideas about the extinction make this a fascinating look at experts confronting profound and distant mysteries.
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Inside This Book (learn more)
First Sentence:
Early Triassic rocks are boring. Read the first page
Key Phrases - Statistically Improbable Phrases (SIPs): (learn more)
million years ago plus, fungal spike, chessboard model, evolutionary fauna, volcanic ash beds, sic boundary, flood basalts, biotic recovery, conodont zones, carbon isotope shift, carbon isotopic record, marine revolution, fossil zones, carbon shift, massive volcanism, strontium ratio, shocked quartz, biotic recoveries, extraterrestrial impact, marine extinction, mass extinction, extinction scenarios, rugose corals, survival interval, greater extinction
Key Phrases - Capitalized Phrases (CAPs): (learn more)
Early Triassic, Middle Triassic, South Africa, Jack Sepkoski, United States, Late Devonian, Andy Knoll, Paul Wignall, Sam Bowring, Lootsberg Pass, Cape Fold Belt, Late Cretaceous, Early Cambrian, Graphite Peak, Mount Pinatubo, North America, University of California, Early Permian, Ural Mountains, Geological Survey, John Phillips, Late Triassic, New York, Time Figure, Bowen Basin
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