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by Andrew H. Knoll

  • ISBN: 0691009783
  • Category: Math & Science
  • Author: Andrew H. Knoll
  • Subcategory: Biological Sciences
  • Other formats: txt lrf docx lit
  • Language: English
  • Publisher: Princeton University Press (April 6, 2003)
  • Pages: 288 pages
  • FB2 size: 1605 kb
  • EPUB size: 1492 kb
  • Rating: 4.6
  • Votes: 793
Download Life on a Young Planet: The First Three Billion Years of Evolution on Earth fb2

Life on a Young Planet book. Andrew H. Knoll is a paleontologist who is particularly conversant with the integrative approaches of modern day evolutionary science.

Life on a Young Planet book. Rooted in the rocks, he writes with skill about the geological and geophysical processes at work in early earth formation, and their implications for the evolution of life. He explains the complex geochemistry that became, in time, a biochemistry.

The Earth of three and one half billion years ago was different from the one we live in but not quite unrecognizably so. Oceans and continents already existed, and had for 700 million years previously.

Life on a Young Planet by Andrew Knoll: What a brilliant book. Everything you could possibly want to know about the history of the planet and life on it, beautifully, clearly and succinctly explained. I will probably reread this book just to absorb nuances I lost in the first reading. The author explains different opinions on all the divisive topics (like snowball earth) in a fair way and with a kind of organized thinking that's impressive too. And yet he manages to be completely entertaining. And, the author has no agenda (which ruins a book for me).

Andrew Knoll explores the deep history of life from its origins on a young planet to the incredible Cambrian .

Andrew Knoll explores the deep history of life from its origins on a young planet to the incredible Cambrian explosion, presenting a compelling new explanation for the emergence of biological novelty. In laying bare Earth's deepest biological roots, Life on a Young Planet helps us understand our own place in the universe-and our responsibility as stewards of a world four billion years in the making.

Read unlimited books and audiobooks on the web, iPad, iPhone and Android. Andrew Knoll explores the deep history of life from its origins on a young planet to the incredible Cambrian explosion, presenting a compelling new explanation for the emergence of biological novelty. The very latest discoveries in paleontology-many of them made by the author and his students-are integrated with emerging insights from molecular biology and earth system science to forge a broad understanding of how the biological diversity that surrounds us came to be.

2004 - "Life on a Young Planet: The First Three Billion Years of Evolution on Earth". 2014) Paleobiological perspectives on early eukaryotic evolution. Cold Spring Harbor Perspectives in Biology, doi: 1. 101/cshperspect. Princeton University Press, Princeton NJ, 277pp. Knoll (2013) Oxygen, ecology, and the Cambrian radiation of animals. Proceedings of the National Academy of Sciences, USA 110: 13446-13451. Petroff (2013) The meaning of stromatolites.

Presumably about 4,500 million years ago, our planet became a solid object and the Earth/moon system formed.

Article in BioEssays 28(4):438-439 · April 2006 with 13 Reads. How we measure 'reads'. Presumably about 4,500 million years ago, our planet became a solid object and the Earth/moon system formed.

Australopithecines, dinosaurs, trilobites--such fossils conjure up images of lost worlds filled with vanished organisms. But in the full history of life, ancient animals, even the trilobites, form only the half-billion-year tip of a nearly four-billion-year iceberg. Andrew Knoll explores the deep history of life from its origins on a young planet to the incredible Cambrian explosion, presenting a compelling new explanation for the emergence of biological novelty.

The very latest discoveries in paleontology--many of them made by the author and his students--are integrated with emerging insights from molecular biology and earth system science to forge a broad understanding of how the biological diversity that surrounds us came to be. Moving from Siberia to Namibia to the Bahamas, Knoll shows how life and environment have evolved together through Earth's history. Innovations in biology have helped shape our air and oceans, and, just as surely, environmental change has influenced the course of evolution, repeatedly closing off opportunities for some species while opening avenues for others.

Readers go into the field to confront fossils, enter the lab to discern the inner workings of cells, and alight on Mars to ask how our terrestrial experience can guide exploration for life beyond our planet. Along the way, Knoll brings us up-to-date on some of science's hottest questions, from the oldest fossils and claims of life beyond the Earth to the hypothesis of global glaciation and Knoll's own unifying concept of ''permissive ecology.''

In laying bare Earth's deepest biological roots, Life on a Young Planet helps us understand our own place in the universe--and our responsibility as stewards of a world four billion years in the making.


Reviews about Life on a Young Planet: The First Three Billion Years of Evolution on Earth (7):
Maman
Andrew H. Knoll's Life on a Young Planet: The First Three Billion Years of Evolution on Earth is one of those rare books that can change your, or at any rate, my, picture of reality.

Dinosaurs and mastodons don't wander through these pages, unless you count a cameo or two. Their time was still far in the future when the characters whose story is told here held center stage. The Cambrian Period, which started about 543 million years ago, or a bit less than ten thousand times as long ago as our own species originated, ushered in the Paleozoic Era and the first easily recognizable fossils. It was the first age of animals - not the very first animals, but the first animals with considerable size and complexity. All the animal phyla we now recognize were onstage in the Cambrian, as well as numerous phyla dead and gone. Before the Cambrian, only sponges, jellyfish and other very simple animals left any trace. The three billion years of the fossil record preceding the Cambrian are Knoll's subject, and it is unexpectedly fascinating. A couple of chapters feature the Cambrian, but mainly it looms as an offstage presence, foreshadowed more than depicted.

Knoll is a graceful and vivid writer, and the story he tells is a detective story, as most good science stories should be (and why does that part always get lost in science textbooks, especially those for kids?). The web of evidence from which the past is constructed is an intricate one, built out of chemistry, physics, and biology, classical and molecular, but above all, out of old rock and the traces left on it by life. Because of that intricacy, the book makes some demands on the reader's attention span and memory for pattern, and enough background in biology to know the difference between Eukaryote and Prokaryote would be useful.

The Earth of three and one half billion years ago was different from the one we live in but not quite unrecognizably so. Oceans and continents already existed, and had for 700 million years previously. Those continents have left little of themselves behind though, suggesting, says Knoll, that the great geological engine of plate tectonics might have worked differently in those younger and internally hotter days; able, perhaps, to swallow and digest continents as well as oceanic crust. The earliest, highly suggestive but not quite conclusive, evidence of life dates from then.

Of what does that evidence consist? Microscopic impressions in the rock and organic remains of possible life, and context, context, context. Paleontology is a field science, and paleontologists spend an exciting part of their time clinging to precarious and sometimes icebound cliffs to retrieve their samples, but it is now also a laboratory science. The rocks containing these traces must be sliced in thin transparent sections, scrutinized through powerfull microscopes, subjected to isotopic analysis in a mass spectrograph - life, it seems, is picky about the carbon (and other element) isotopes it uses, and that signature is one of the most definitive. Knoll tells of putting the crucial samples under the microscope, scrutinizing them, and in the end concluding that while a circumstantial case existed, it couldn't be considered conclusive.

A deep skepticism of both one's own ideas and those of others is indispensible in this most vital kind of science. Knoll is expecially good at presenting contrasting ideas and hypotheses - a breath of fresh air after listening to the narrow minded fanaticism of some of the string theory debates. Paleontologists, of course, have a big advantage - they have actual evidence.

A few hundred million years later, the evidence becomes more unambiguous. Casts in the rock preserve more detail, both morphological and biogeochemical. Life, too, becomes more elaborate and presents more features for recognition. The cyanobacteria are one of the main heroes of the story. For two and one half billion years they have thrived almost unchanged - they did much of the heavy lifting of producing the oxygen that was previously lacking in our atmosphere, and they were incorporated in eukaryotic cells to allow plant life to arise.

I won't try to summarize this long elaborate story, but let me mention a couple of themes. Geology set the stage for life, but life became a major player in transforming the atmosphere and the oceans. Occasional cataclysms have shaken and transformed evolution. The photosynthetic production of oxygen was certainly one of these. Others likely had extraterrestial origins - great asteroid impacts, for example. Still others probably originated in the tectonic processes of volcanism and continental drift. Most, like the great ice ages of the late Proterozoic (just before the Cambrian efflorescence) are of uncertain provenance. Those ice ages, incidentally, made the more recent ice ages of the Pleistocene look like midgets. Glaciers advanced even into the tropics, and much, or all, of the ocean surface was frozen to great depths. Cataclysm for one branch of the tree of life may be opportunity for another. Mammals and dinosaurs coexisted for 150 million years, during all of which time the reptiles were clearly dominant. Not until the asteroid wiped out the dinosaurs did the great mammalian expansion happen. Knoll calls this "permissive ecology." When all the good jobs or ecological niches are already taken, it's hard for an evolutionary novelty to get a start.

The penultimate chapter is devoted to paleontology beyond the Earth, and expecially to LAH-84001, the grapefruit sized meteorite from Mars that NASA in 1996 claimed showed evidence of life. His exceptionally clear prose is put to good use explaining the pros and cons, as well as crucial background material (how do we know it came from Mars, for example - it was found in Antarctica.) The years since of intense study of this meteorite have taught science a lot about how to look for signs of life from other planets, but have not been kind to NASA's claim. The claim has not been disproven, but all the lines of evidence upon which NASA made the claim have been cast into doubt.

The final chapter, or epilogue is truly an elegant essay in itself. He touches on many themes, from religion and science to creationism, but concludes with an appeal that we realize the implication of the fact that we, the human race, now play a major role in shaping the future of the planet.

If we can acknowledge our unprecedented role as planetary stewards, we may be able to discharge our responsibility with wisdom and with honor. On this issue, at least, faith and science find common ground. I don't know whether God decreed the passenger pigeon, but if He did, it was not for us to exterminate...

Through our actions or inaction, we decide the world that our grandchildren and great grandchildren will know. Let us have the grace and humility to choose well.

He includes an extensive and lightly annotated list of references and further reading. In case it wasn't obvious, I really liked the book.
Wel
Life on a Young Planet: the First Three Billion Years of Evolution on Earth is an enjoyable overview of what has been discovered about the very beginnings of life. For those of you who haven't studied biology for over 20 or 30 years, it will come as something as a surprise how greatly the "lower" levels of life's tree have changed since you went to high school.

Most of those interested in paleontology are aware of the conundrum posed by the apparent lack of evidence for the early stages of life's development. The pre-Cambrian was literally a blank slate for most of the decades since Darwin first suggested that soft bodied forms probably preceded the fossilized life forms we find in the geological record. Most of you will also be familiar with Stanley Miller's research which produced molecules similar to those expected of pre-life in his famous flask experiment. With this and the growing information arising from DNA studies and with the discovery of halophiles and thermophiles in out of the way places, even more has been detailed. The relationships of various extant and extinct life forms has been clarified to a far greater extent. A revamping of the earlier Linean tree of relationships and a clearer surmise as to the stages through which first pre-life and then prokarytoes passed on their way to eukaryotic forms is also much clearer. The author gives a very lucid explanation of the chemistry of life with respect to the earth's early atmosphere and ocean chemistry.

Although some of the information is a rehash of material, the author has had the advantage of working in regions where early life forms were probably first developing and in regions that had been off limits to western researchers in the past. More and more as data from former communist countries and the West is pooled and an exchange of ideas is encouraged, one can see the speed of learning increase in every field. Paleontology is no exception.

A wonderful book, pushing the limits of knowledge a little further.
Granijurus
Well written to the point of wanting to see what happens next, as in a novel. Whether it is paleontology or evolution that peaks your interest you will be happily engrossed in this book. If you don't have a background in the life sciences and want something more in-depth than Nova, this is the book. If you do have a background in the life sciences this book is an excellent way to understand how life evolved from one of the best paleontologists.
Dominator
Want to know about the earliest living things? Read this book. The writing style is direct but lively with appropriate allusions to popular culture. Some of the topics are highly controversial and Knoll does a great job of telling you the relevant facts so you can reach your own opinion. For this alone, I would give the book 10 stars if I could. Still I wish it had more illustrations and a better description of how research is conducted and how rocks are analyzed. Potential readers should be warned that Knoll assumes the reader is generally knowledgeable about Biology and scientific terminology.
Zargelynd
Very deep reading material, for me anyway. What I could understand was quite good. It did make me realize just how much ecology is involved in the evolutionary process. If you are a second year college student in earth science you might want to read this. The illustrations and photos were very helpful, when I could find out which ones the author was talking about.
NI_Rak
Life on a Young Planet covers a (very long) period that is pretty much a closed book to most amateur paleontologists. Andrew Knoll does an excellent job of taking us through the aeons while making the story of life as interesting as it is important. While there are facts and figures to satisfy those in the know about early life, Knoll dumbs it down for the rest of us to a point where it can be hard to put the book down. Highly recommended for anyone who wants to expand their knowledge of earth bioscience back beyond the dinosaurs or even the Burgess Shale.

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