Ichthyosaurs

Ichthyosaurs painted by Heinrich Harder (1916)

History of Life
(Geology 100)
Department of Geology, The College of Wooster
Spring 2008

Preparation Questions

Latest Quiz Key

Sample Test

Geology Course Pages

Welcome to the webpage for the History of Life course at The College of Wooster! You will find here our syllabus (a "living syllabus" which is added to every week) and the details of the course itself. For each week's topics I post links, images and other items to provide additional information (and alternative views) as we explore the wonders of life's history through the semester. This page is essentially a required blog for the course, as well as a set of resources we will use in class. To keep our material as up-to-date as possible, I post supplementary information only a week in advance. I thus expect registered students in the course to visit this site at least once a week. If you have ideas about items you would like to see posted here, please send me e-mail (mwilson@wooster.edu) or talk to me in class. I hope you enjoy the course! You may also want to visit our "Invertebrate Paleontology at Wooster" general page, our Invertebrate Paleontology course page, and our Paleontology Independent Study webpages.

Mark A. Wilson
Department of Geology
The College of Wooster
Wooster, OH 44691 USA
mwilson@wooster.edu


Schedule of Lectures
(With Weekly Links to Other Web Resources)
 
Lectures are in Scovel Hall Room 105 on Mondays, Wednesdays and Fridays from 8:00 - 8:50 a.m.

January 14-18

Antiquity of the Earth and Life (Geologic Time and the Fossil Record)
Recommended Reading: W&M pages 1-15, 60-76
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #1:

Geologic time is a fascinating topic. It is so unimaginably long it has been called "deep time". Please learn the Geologic Time Scale as soon as possible because it is the chronological language of this course. Here is a clever test you can take on the Web when you think you've learned the terms. If you want to see ALL the time terms geologists use, check out this PDF of the geological time scale. You need to know only the eras, periods, and Tertiary and Quaternary epochs. William Smith was an Englishman responsible in many ways for the principles behind our use of geologic time. James Hutton was a Scot who first effectively described and applied the concept of "uniformitarianism" in geology, which requires vast amounts of time. NOTE: Because the required terms of the Geological Time Scale for this class are unclear from the above links, I've posted a MicroSoft Word version of our time scale as well as our own pdf version. You will see that I recognize the Ediacaran Period before the Cambrian.

Geologists distinguish between relative and absolute time, with the first being the ordering of events, and the second using measurements of time. We will most often use relative time (such as the "Cambrian Period") in this course, but also occasionally cite absolute time ("65 million years ago").

The concepts of radioactive decay and its use in the dating of Earth materials take some time to master. The University of Waikato in New Zealand has an excellent explanatory website on radioactive dating. On this site called "popcorn" you will see an Applet display of decay demonstrating its spontaneity and constant rate. (It loads slowly but is worth it.) A more detailed explanation of how half-lives are really calculated is shown here. See what I have spared you?

As an introduction to the fun of paleontology, there are plenty of dinosaur animation sites on the Web. Try searching for "dinosaur" on YouTube and you'll get thousands of odd videos! (Including, of course, "Walk the Dinosaur" of happy memory.) You will also want to visit The Paleontology Portal which is "a central entryway to paleontology on the Web". It is an excellent link to thousands of paleontological resources.

You are in a course on a scientific topic which has a dedicated opposition. Most "young earth creationists" believe that the Earth and the Universe are at most a few thousand years old, which is radically different from the billions of years cited by scientists (scientists like me). Their arguments appear scientific, but you will quickly see that they are based on misconceptions, misrepresentations, mysteries and zealotry. Take a look at this page of links citing "evidence for a young Earth" from Answers in Genesis. These are the people who are the proud producers of the multimillion-dollar Creation Museum in Kentucky. We will often list here links to creationist resources so that you are not surprised by the controversies stirred up by a course on the History of Life. Don't confuse their work with real science.

Geology in the News:

A new report from the National Academy of Sciences emphasizes the importance of teaching evolution in the public schools. This is an everlasting debate in this country. the issues were hot when I was in high school, and they've remained so. I'll be interested to hear how much evolutionary education you've had prior to this course.

I hope you also learn through your college education how to assess a science news story. Take this one: "Biting Insects May Have Killed Off Dinosaurs". Look carefully at the premises, which include "dinosaurs declined and disappeared over a period of hundreds of thousands, or even millions of years" (false). Look at the evidence: a biting insect found in Late Cretaceous amber which may have carried a disease. Wonder why no dinosaur paleontologists are involved with this story!

Here's a report on a remarkable Cretaceous dinosaur fossil (Psittacosaurus) found recently in China which gives us evidence of how its skin was constructed. It was apparently attacked by another dinosaur and its torn skin preserved by rapid burial.

A new 48-million-year old fossil (the deer-like Indohyus)was found in the Kashmir region in India which is yet another link between land-dwelling animals and the cetaceans (whales and dolphins). We will resist the temptation to call such fossils "missing links", primarily because there are always by definition links missing in fossil lineages. A cool story, the origin of whales and dolphins. You'll hear it much later.


January 21-25

Mechanisms of Organic Change: Evolution
Recommended Reading: W&M pages 122-146
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #2:

This week we begin discussing evolution. (The "e word" as a high school administrator once told me.) Start with a good definition of evolution, for you will soon see that most dorm room conversations on the topic usually have significant errors and misconceptions. You can then visit "Frequently Asked Questions About Evolution" at TalkOrigins Archive. The University of California Museum of Paleontology at Berkeley has an excellent website on the history of evolutionary theory, including good sections on pre-Darwinian thinkers. The Berkeley pages on "Understanding Evolution" are the best on the web. Charles Darwin is well represented on the Web, and Alfred Russel Wallace is the subject of this excellent website by Charles Smith of Western Kentucky University (who also has a useful site entitled "Early Classics in Biogeography, Distribution, and Diversity Studies: To 1950".) The full text of Darwin's most famous work, The Origin of Species, is available on-line. It is not scintillating reading, at least not on a computer, but you may want to peruse the preface and the conclusions. Another good general source for concepts of evolution is the recently-written "Teaching About Evolution and the Nature of Science" by the National Academy of Sciences.

The public opposition to evolutionary theory is deep and strong in this country, and it has spread internationally. Anti-evolutionists are very diverse, and many of their beliefs are mutually contradictory. Here is a graphical and textual classification of beliefs on origins and evolution. I maintain a webpage on "The New Creationists", which contains links to anti-evolution sites. Please do not misunderstand me: I believe that "Scientific Creationism" and other anti-evolution movements are founded on nonsense, ignorance, wishful thinking and a deep undercurrent of anti-intellectualism, but they are part of democracy's fabric and the public discourse on science. We should listen to them closely and try to understand the social and political forces behind their strong beliefs (and still vigorously teach evolution). Some creationist websites are very sophisticated, such as that of the Institute for Creation Research and Answers In Genesis (AiG). (Three years ago I debated Mr. Ken Ham of AiG on a radio talk show in New York City. That was an experience.) These sites and others provide easy access to the primary tenets of scientific creationism. I especially recommend the questions-and-answers page of AiG and the Handy-Dandy Evolution Refuter. The National Center for Science Education (NCSE) is the best known defender of evolution in American public schools. The Creation-Evolution Reference Database is a good place to start for anyone who wishes to study this topic in detail, although it is no longer updated. The American Scientific Affiliation is dedicated to the simple and seemingly obvious observation that scientists with religious faiths need not be creationists.

For an insight into the most recent political implications of anti-evolutionism, you can't do better than to read the opinion of Judge John E. Jones in the recent Dover, Pennsylvania, "Intelligent Design" court case (a long pdf).

For more information on the rock and fossil samples you received last week, you can go first to this webpage on Indiana geology for information on the rock itself and its context (found with a Google search on "bedrock" and "Indiana"), and this webpage for photos and descriptions of the typical fossils in these rocks. This is some of the most fossiliferous rock in the world.

Geology in the News:

The largest rodent known has been found as a fossil in Uruguay. How large, you ask? The size of a bull, and weighing a full ton. Big enough. It is four million years old.

This story comes from my graduate alma mater: The reproductive age of dinosaurs has been estimated by paleontologists at the University of California, Berkeley. (Here is their colorful press release.) Some species, at least, were sexually mature at 8, 10 and 18 years, which is earlier than previously thought. I also learned here that dinosaur life spans were from 30 to 60 years. You've got to love the news media title for this article: "Dinosaurs Had Adolescent Sex, Study Finds".

Here's a story on that massive volcanic eruption in Colombia that I told you about in class. The Galeras volcano (which is over 14,000 feet high) has forced the evacuation of thousands of people.

The NASA spacecraft Messenger has sent back amazing new photos of the surface of Mercury, including views of craters as small as 300 meters across. These images will tell us much about the violence of the early Solar System, when the Earth also received many large blows from meteorites. The Europeans and Japanese are working on another space probe which will visit Mercury in 2019. These marvelous machines must be built to withstand temperatures from near absolute zero to 350°C.

Here's a story of a fossil whale skull embedded in sandstone ... and red tape ... in southern California. The find is curious in that hikers walked over it for years, but not headline material. I was most interested to learn that Orange County has an official paleontologist!


Jan 28 - Feb 1

The Very Beginning: Origin of the Universe, the Early Earth & Life
Recommended Reading: W&M pages 147-165
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #3:

The Big Bang Hypothesis is an extraordinary concept. Readable, albeit short, explanations of Big Bang ideas can be found at "Stephen Hawking's Universe", and another much more extensive set of resources at "Hot Big Bang". Given your first preparation question, you will want to especially see the page on the awesome singularity. Want an artist's view of the Big Bang? For you humanities majors, how about Big Bang Philosophy? You can ponder many universes beyond the Big Bang with Stephen Hawking. And it wouldn't be the web without a site like "The Big Bang is Wrong!" For those of you looking for a simple red shift explanation, click away here or on this other simple red shift webpage from PBS. The last even has an exercise you can try. There is a very cool Big Bang animation on this French website; I may use it in class (despite the French). I'm not sure what the point is of this next Big Bang animation, unless it is to make us feel insignificant.

This star formation site is good, but also very technical. Here's a JPL-NASA planet formation site with "artist's conception" images and a movie you can download. Some exquisite photographs of the Moon's surface are also posted by NASA. This webpage from NOVA has superb animations of the "Big Whack" hypothesis for the origin of the Moon.

An astronomer named Neil Comins wrote an interesting little book called "What if the Moon Didn't Exist?" The Moon is critical to the maintenance of life on Earth, which I find amazing. Also, here is the homepage of NASA's brilliant "Stardust" project, which brought to Earth the "dust" of a comet. Now you know the importance of this study to our ideas about the origin of the solar system, for comets are samples of the original nebula frozen in time.

Now for the complex and contentious ideas about the origin of life. "How life emerged" is a huge site with all sorts of interesting essays and illustrations. (Unfortunately it is also belabored by too many animations and sound effects. Fortunately for you I haven't figured out how to do these yet!) Our friends in the Chemistry department at Beloit College have this origins webpage with animations of the Miller-Urey experiment. (Here's the nice animated Miller-Urey experiment webpage I may use in class.) The Creationist opposition to all naturalistic theories for the origin of life is characteristically strong, but their slick webpages have numerous errors. Don't forget those panspermians who avoid the issue of origins altogether -- they say life came from space, where it always was!

If you are interested in being on the e-mailing list for the Department of Geology, please send me a note (mwilson@wooster.edu). Our list has the names of students who enjoy geology, maybe to the point of considering it as a major. You will receive departmental announcements about upcoming lectures, picnics, field trips, and internship opportunities.

Geology in the News:

Here's a good start for geology-in-the-news for this week: Bigfoot on Mars! Don't believe me? Just check out the photo. It is so obvious. Sure, there are spoilers who want you to believe this is just a rock and a trick of the light, but what are they trying to hide? Sure it is very, very small, but Mars is a small planet, after all. What else is the government hiding?

(Just making sure you know satire and cynicism when you see it from me. Professors have to be careful with such things! My credentials and feelings on the topic are probably best shown by this FYS course syllabus.)

It should not be news to you that the Earth's climate is "clearly out of balance" and that human activities play a strong role in the changes. It is now reinforced with an official statement from the American Geophysical Union. We are now in the position of asking what we can realistically do about it. (I'm in the lower-emissions-but-also-adapt school.)

Did you know that women have a slightly different vertebra which enables them to better carry the baby during pregnancy? This wedge-shaped lower vertebra is found only in human females and our immediate bipedal ancestors. A cool example of selection and adaptation.


February 4-8

The First Record: The Oldest Fossils
Recommended Reading: W&M pages 178-185
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #4:

Our week will begin with continued discussions of origins, especially hypotheses about the origin of life. Please be sure to look at the links listed for last week on this topic. We will also look at the earliest fossil record, which now goes back to just over 3.8 billion years. The University of Arizona has a nice page on the six kingdoms of life, which makes a good starting point. Another website to examine would be the one on fossil bacteria at the University of California, Berkeley. This site also has an excellent page on cyanobacteria and stromatolites, which are the first easily-recognized fossils. Check out their Archean page, though, and find the critical error! (It is in the first paragraph.) Here is another stromatolite page. Queen's University in Ontario also has a good early life online museum website. There is chemical evidence for life which even predates the oldest stromatolites. In fact, the NASA page on the origins of life is especially good for finding additional links. For an excellent short summary of "the emergence of complex life", you can't beat this colorful page from the University of Michigan.

I recently learned of the discovery of a very large virus named Mimivirus. (I'm apparently about four years behind on this one!) This virus is extraordinary: it is larger than some small bacteria, and it has over 1200 genes. It blurs the distinction between life and non-life (like all viruses) and may well represent a fourth domain of life. It may even tell us that viruses, far from being derivative parasites, may actually be the primary life form from which all else evolved. This is the most exciting news I've heard on the origin of life issue for years. When we learn that most of the genetic material on Earth is held by the viruses, we must consider that maybe we're overlooking a big story! For more on Mimivirus and other similar topics, you can't beat the aptly-named giantvirus.org.

We are now beginning to order geological and evolutionary events in time. You might want to refer to this annotated timeline as a reference. Do not take it too literally, though, because there are some events either not recorded or now known to have occurred at different times. Again, the events you should be most concerned about are those we cover in our lectures.

Geology in the News:

Heather Hunt sent this one: Some geologists believe that people have made such a difference to the environments and climate on Earth that we actually ended the Holocene Epoch and have started the Anthropocene. Don't throw away those old time scales yet, though. I suspect the Holocene will last a bit longer than these people think, especially when the next and inevitable Ice Age is upon us.

You've got to see the photo of this new mammal discovered: an elephant shrew in Tanzania. Elephant shrew? You'll just have to see it. Another indication of just how much there is out there still to find. These are the best days to be a scientist.

The NASA spacecraft Messenger is producing more images of Mercury, many of which show its volcanic history. I love that mysterious "spider-crater" complex.

New evidence from the Cretaceous-Tertiary crater in Chicxulub shows that the dinosaur-killing meteorite struck in deeper water than previously assumed. There is also now better evidence from the crater for reconstructing just what kind of dust, gas and debris was sent into the atmosphere from that impact. This is one of the best stories in science, and we just keep learning more.


February 11-15

Developing Marine Ecosystems
Recommended Reading: W&M pages 231-248
Special Events:
Assignments: First Lecture Exam (February 15) (Preparation questions)

Web Resources for Week #5:

Our topic this week is the rise of animal life on Earth, and the early development of marine communities. A good place to start on the Web is Berkeley's "Vendian Animals" page with its many illustrations and links (in class we will refer to this time interval as the "Ediacaran"). Queen's University of Canada also has a good Ediacaran fauna page. (Canadians are big on the Precambrian.) There is also a very professional Ediacaran Page from an amateur in New Zealand. His Cambrian and Ordovician pages are excellent as well. We will spend considerable time on the rise of skeleton-bearing invertebrates in the Cambrian. Please visit Berkeley's Cambrian page, especially their subpage on the "Tommotian" (the earliest Cambrian). I hope you will be fascinated with the Burgess Shale (this is the Smithsonian's main page on it), found in the Middle Cambrian. This is the Smithsonian's Burgess Shale reconstruction image. A site called "Prehistoric World" has some great little Burgess Shale animations. The Cambrian also was the most important time for those fascinating little critters, trilobites. You can join the Yahoo Trilobite Club if you like and have access to an extraordinary number of images and links for these extinct animals. The "Palace of Trilobites" (these people are VERY enthusiastic) is in Japanese, but the universal binomial nomenclature and beautiful images will help you out. There are many more of these out there in cyberspace. For some photographs and brief studies of Ordovician fossils in the Cincinnati area, you can't do better than Wooster's own "Keck Ohio" pages (although they are getting a bit dated in this fast-paced webworld). The Palaeos webpages on the Ordovician are very well done and updated often.

Here is sample test #1 for your preparation. Remember that the test will begin at 7:55 a.m. on Friday. Don't forget to know the Geologic Time Scale so well you can recite it in your sleep. It will be the last problem on your test.

Geology in the News:

Maybe a tad of good news here when it comes to global warming: the oceans may have a sort of "natural thermostat" to keep them from warming too much to kill off tropical corals. Natural processes, such as evaporation, may keep water cooler than 31°C. Still, warming water is currently killing corals which live in cooler conditions.

How did large dinosaurs get enough nutrition for their bulk when we know they ate poor foods like ginkgo leaves and ferns? Recent experiments with fermentation and stomach bacteria show that it is possible they got plenty of the right stuff from these plants given the right amount of time and chemistry in the gut.

Horseshoe crabs are now even older than we thought -- about 100 million years older. New finds in Ordovician rocks in Canada show that this hardy clade has survived even more of the hazards of life to make it to us today in basically the same form. Remarkable.

"Star eats star and builds planets from the crumbs." Can't beat that headline! Looks like it's true, too. Another way in which we can develop planet-forming materials and conditions, thanks to the Hubble Space Telescope and the Chandra X-Ray Satellite.

 


February 18-22

Plate Tectonics
Recommended Reading: W&M pages 35-59
Special Events:
Assignments:

Web Resources for Week #6:

Our primary topic this week is the Theory of Plate Tectonics, with an emphasis on how the dynamic Earth has affected the evolution of life. We can start with this beautiful world map, showing continents, mountains, ridges, transform faults and trenches in the Pacific and Atlantic Oceans. Here are some maps of the ancient Earth, with helpful color coding. This site (from an astronomical observatory in South Africa) has a good long page summary of plate tectonic theory. (It is a bit slow, but worth the wait.) NASA can show us by satellite laser ranging data the modern rates of plate movement. (One of my brothers used to work on this project.) The Nevada Seismological Laboratory at the University of Nevada, Reno, has an excellent page on plate tectonics and earthquakes. And who would have guessed that by just typing in the address "www.platetectonics.com" we could find such a beautiful set of graphics and text? This is an extraordinary site, complete with on-line research articles. The University of Texas hosts The Plates Project which concentrates on producing accurate plate reconstructions of the past. Of course, plate tectonics is an ideal subject for web animations. PBS reviews plate tectonic theory with a simple and clear set of images and animations. Here is a global history of continental movement in the last 750 million years from UC Berkeley. The University of Kentucky has some very cool animations of the last 150 million years you control with the cursor. This page also takes a few seconds to load because of the sophisticated graphics.

As for the primary effect of plate tectonics on us, visit the real-time global earthquake website maintained by the U.S. Geological Survey. You will see how very common earthquakes are around the world, and where you do not want to buy a house. You can further investigate temblors at The Virtual Earthquake website. PBS has a nice set of animations of earthquakes from a global perspective, along with volcanoes and the geological phenomenon we now know all too well, tsunamis. (Here is a summary page on the devastating 2004 tsunami in the Indian Ocean.)

This week we also begin a discussion of the causes of the Permian Mass Extinctions -- the greatest disaster in the History of Life. An excellent website is this one from England on the Permian Extinctions, complete with a discussion of an impact as a possible cause. Paleogeographic maps of Pangaea at the end of the Permian can be found on the Scotese website (note that it was not "99% of all life" which went extinct) and on the Permian Page from Northern Arizona University. Wikipedia has a good Permian Extinctions article, although the topic is controversial enough that some parts of it may be edited by partisans of one cause or another.

The first test results: the score range is 35-100% (quite a spread), and the average is 81% (which is good).

Geology in the News:

Andy Knoll, a paleontologist at Harvard, has excellent evidence that Mars water, when it existed in liquid form, was far too salty for life. Or, as someone will inevitably qualify it, "for life as we know it". I'm never surprised that there is as yet no evidence for life on the other planets we know. The chances of life taking root elsewhere in our solar system are very low.

Take a look at this marvelous fossil bat found in Wyoming rocks about 25.5 million years old. That's the kind of fossil I'd like to find! It shows that bats appeared in their present form before they could echolocate, which has been a persistent question about their evolution.

Rob McConnell told me about this story: tiny little pterodactyls discovered in China. Little Nemicolopterus crypticus is very cute. The specimens found are not adults, so we don't know how much more they could have grown. They are 120 million years old.

A "freakish" new duckbill dinosaur was found in the Upper Cretaceous of Mexico recently. Velafrons coahuilensis doesn't look so odd to me. It had a beautiful set of expanded nasal cavities probably used for making magnificent (and loud) sounds.


February 25-29

From Fins to Feet: Early Vertebrate Evolution
Recommended Reading: W&M pages 234-242
Special Events: Osgood Lecture (Paul Olsen) on Wednesday, February 27, at 7:30 p.m. in Lean Lecture Room (Wishart Hall); “Mega Eruptions, Mega Impacts, Mass Extinctions, and the Shape of Life”; this is a required class lecture.
Assignments: (Preparation questions)

Web Resources for Week #7:

Vertebrates! At last, our cousins appear. The best place on the Web for simple and thorough descriptions of the chordates and their history is at the University of California Museum of Paleontology. Check out their pages on the urochordates (tunicates), cephalochordates, and chordates in general. The Berkeley tetrapod (four-legged) webpage is especially useful for us. This page on limb evolution from an anti-creationist website is very useful, even if the illustrations are a bit clunky. I like this website lovingly devoted to the ancient coelacanth fish Latimeria. It has many illustrations and an extensive history of what we know about this remarkable evolutionary survivor. The Tree of Life page on terrestrial vertebrates will show you current ideas about the relationships of fish and early amphibians. It is a rich source of further links. Our class lecture outline on the early vertebrates is found here. I'm giving this to you directly not to replace your notes but to give you a thorough and concise source for the concepts and vocabulary.

Here is a good general page from Norway on amphibians. Berkeley also has an amphibian page, but it is considerably shorter. If you're looking for a lot of frog images, look no further. If you want to freak out your roommate right now, try amplifying a few frog calls from your computer.

Geology in the News:

John Sime was the first to send in a link to the news about a giant frog from the Late Cretaceous of Madagascar. Very impressive. Note that it also tells us something about the plate tectonic situation in that part of Africa at the end of the Mesozoic. Here's another link to the story in case the above New York Times webpage becomes unavailable. And a delicious quote from the BBC on the monster frog: "Its diet would most likely have consisted of insects and small vertebrates like lizards, but it's not impossible that Beelzebufo might even have munched on hatchling or juvenile dinosaurs."

Yet more new dinosaurs found, these from the Cretaceous of the Sahara. You've got to love the description of one of them: "Eocarcharia could rip off limbs and gash open prey with its blade-like teeth. It had a long bony eyebrow that gave it a menacing glare, and might even have used its brow bone to butt heads with mating competitors." Now that's a dinosaur.

Last week's lunar eclipse was fantastic, and a rare sight in the dodgy skies of northern Ohio. The color was very impressive, at least in some parts of the world. We won't have such show again until December 20, 2010.

Stepped alluvial fans (or deltas) on Mars are more evidence that the Red Planet once had liquid water on its surface. This wasn't a system like we have on Earth, however, since this water seems to have come in pulses and from an internal source rather than the atmosphere. Note that this investigation involves space probe images combined with experiments on Earth.


March 3-7

The Amniotic Egg: Amphibians to Reptiles
Recommended Reading: W&M pages 242-245
Special Events: James Kennett Lecture (Thursday, 7:00 p.m., Lean Lecture Room, Wishart Hall); required
Assignments: (Preparation questions)

Web Resources for Week #8:

The eighth week already. It must be time to really "conquer the land" as we say too often. The reptiles are an enormously successful class, and their diversity is reflected in the websites devoted to them. I can only give you links to a few of the many groups we will discuss in class this week. (Just wait until we get to the dinosaurs!) You will want to review the wonders of the amniotic egg. For the technically inclined, here's a complex page designed for those studying the amniotes. Here's an introductory page to the turtles (anapsid reptiles), and then another for the diapsids. One of our favorite synapsids is the reptile Dimetrodon. Here's a Dimetrodon image, a coloring page to print out (for your little brothers and sisters). Everything you want to know about the therapsids ("mammal-like reptiles") can be found here. To round out our initial survey of early reptiles, here is the "living fossil" tuatara. The best general reptile page I've found is from Heidelberg, Germany. It has many very informative (and richly illustrated) pages in English. I'm sure you'll like this mosasaur page from the South Dakota School of Mines and Technology Museum of Geology. I enjoyed this page on Cretaceous marine life from the University of Nebraska State Museum in Lincoln, Nebraska.

A pivotal event in Mesozoic reptile evolution was the Triassic mass extinction, which is well covered on this webpage from the University of Bristol. The rise of the dinosaurs starts soon after. A set of more technical links to the Triassic extinctions has been put together by a German paleobotanist at the Universität Würzburg.

You need some silly links to ease you into Spring Break. This is fruitcake pseudoscience, but you'd be surprised how many people believe these things. Some crackpots, for example, look at the evidence for plate tectonics and instead turn it into proof of an expanding earth? Crazy talk. These guys always sound a bit desperate, craving scientific approval. An expanding earth, by the way, is the only way some people can explain the "surprisingly massive sizes" of dinosaurs. Here are some very nicely done videos of the expanding earth concept by a Neal Adams. You're supposed to give these to your geology professors to show what fools they've been. This guy is fond of satirical, angry letters to scientists, especially geologists, because they just don't seem to recognize his genius. Plate tectonics can't work anyway because the reptiloids of the inner earth wouldn't have their cozy underground caverns for millions of years. The Cretaceous extinctions, as a digression, were not caused by a natural disaster but were instead the result of a war between "two enemy alien groups". Here's something new -- a man working very hard to convince you with NASA photos that there are forests on Mars. All this time the government has been keeping this amazing news from us (while apparently still releasing the photos, silly Feds).

Remember the "scientific creationists"? I hope you haven't forgotten that there is a vigorous political and religious opposition to everything we do in this course. (I'm reminded almost daily in my email.) Compare these two pages: transitional fossil FAQs and the "Handy Dandy Evolution Refuter" on evolution and the fossil record. I hope by now you see the extraordinary flaws in creationist arguments. (My feelings on this issue have grown stronger over the years. Pseudoscience does no one any favors, especially those promoting it.)

Geology in the News:

An incredible pliosaur from the Jurassic of Spitsbergen, Norway, has now been described. This is the largest marine reptile yet known, coming in at an amazing 15 meters in length. Be sure to check out all the photos of this monster, including the one with a child for scale. Extraordinary. I'm not sure that this animal was "big enough to pick up a small car in its jaws and bite it in half", but it certainly could do serious damage. Gotta love the Jurassic.

There was a rare earthquake in the United Kingdom on Wednesday of last week. Although 5.2 seems rather small by California standards, it did some significant damage in some places. A student was injured by a falling chimney. Unfortunately this BBC story has a little graphic on "how earthquakes happen" showing a continental collision. You know well enough that this is not the case for the British Isles.

Erosion in action. Recent storms on the Oregon coast have scoured away beach sands, revealing shipwrecks, old cannons, and strange iron concretionary forms. Up to 17 feet have been removed from some coasts, creating steep scarps. The next storm could well bury it all again in the ever-shifting sands of time. (So poetic.)

Here's a cool story and set of video animations of what we now know about the Moon's South Pole. There may be water ice present in the craters here, and parts of it also receive constant sunlight. Looks like a good place for our first Moonbase to me. The 3-D mapping is especially neat.


March 24-28

Jurassic Park, etc.: The Evolution of Reptiles
Recommended Reading: W&M pages 295-308
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #9:

As you may imagine, the Web is rich with dinosaur pages. Some of these websites are excellent, some are horrible, most are tolerable (and long). Let's begin our explorations at the University of California Museum of Paleontology at Berkeley, which has by far the best dinosaur site. In fact, they invented the concept of the "on-line museum". Start with their general dinosaur page, which has numerous images and links. Then take a guided tour of the Berkeley Dilophosaurus exhibit and their "T. Rex Expo". I suggest ending your Berkeley dinosaur visit with their "Dinobuzz" page which has excellent explanations and discussions of the latest dinosaur research. Other impressive dinosaur websites include that of Paul Sereno, one of the most productive dinosaur paleontologists in the world and virtually an industry to himself. The "Journal of Dinosaur Paleontology" doesn't seem to be a real journal, but it contains some interesting discussions of dinosaur biology. Of course, I hope you've all seen the extraordinary series "Walking With Dinosaurs" on the Discovery Channel. The webpage for this series is superb.

A new link for me: The Dinosaur Interplanetary Gazette (which will keep you busy if you like everything dinosaurian).You might also want to "download-a-dinosaur" to make folded-paper dinosaurs for all your friends. (Notice, though, that some of the dinosaurs listed are not dinosaurs.) The National Geographic website has an excellent presentation on dinosaurs. We cannot forget, of course, all the wonderful evidence that dinosaurs and people lived together. (I hope my sarcasm is apparent.) We'll talk about dinosaur extinction later, but for now you might want to see why the creationists don't believe it was due to an extraterrestrial impact. (If only they could take History of Life, then they'd understand ...) Or, as we said last week, how about the idea that dinosaur size can be explained with an Expanding Earth? I love this craziness!

Here's another creationist page on dinosaurs you must see, beginning with this quotation: "This article will discuss the possibility that there may have been an ongoing effort since the earliest dinosaur 'discoveries' to plant, mix and match bones of various animals, such as crocodiles, alligators, iguanas, giraffes, elephants, cattle, kangaroos, ostriches, emus, dolphins, whales, rhinoceroses, etc. to construct and create a new man-made concept prehistoric animal called the dinosaur." So, apparently this David P. Wozney thinks scientists just made up dinosaurs.

Geology in the News:

The movie 10,000 BC contains many "prehistoric" creatures modeled on actual animals from the Pleistocene. All you have to do is ignore place, time and size!

Here's a cool map (or maybe a warm one) showing the Earth as it was 80 million years ago during the Cretaceous. Not the very high sealevels and lack of ice caps.

There is a hot debate going on right now about the age of the Grand Canyon (and not with creationists). Current estimates are that the Canyon itself is 5-6 million years old, but a recent study suggests it may be up to 17 million years old. It is not an easy question to answer, especially if the early river was much smaller.

Speaking of the Grand Canyon, there has been a recent attempt to restore sand bars and beaches there by releasing water through jet nozzles at 300,000 gallons per second. Imagine the Froude and Reynold's Number equations with this experiment! The water is released through the Glen Canyon Dam. The idea is that its force entrains sand from the bottom of the river and piles it up "naturally" on the sides.

A very impressive avalanche on the surface of Mars has been recorded by an orbiting camera, complete with a huge dustcloud. Events like this make Mars seem that much more real!


March 31 - April 4

Origin of Flight
Recommended Reading: W&M pages 309-310
Special Events:
Assignments: Second Lecture Exam (April 4) (Preparation questions)

Web Resources for Week #10:

Time flies, and now so do vertebrates. We will discuss the origins of vertebrate flight this week. The University of California Museum of Paleontology has an excellent set of pages on flight origins, which includes information on birds, bats and pterosaurs. For details on the latest pterosaur research, try The Pterosaur Database. For more popular questions, you can't beat the Pterosaur FAQs webpage. Wikipedia does a nice job with pterosaurs as well, although you always have to be a bit careful with this source. Stanford University and the National Geographic Society actually want to make a flying replica of a pterosaur. Here's a strange link: "evidence" that pterosaurs lived until the 17th Century, believe it or not. (I suggest "not").

And here is the link to sample test #2 for your enjoyment.

Geology in the News:

Pachycephalosaurs are the bone-headed (or, more charitably, "dome-headed") ornithischian dinosaurs best known for head-butting. A recent study suggests that they did most of this combat as teen-age dinosaurs, or in their adolescent equivalence. Somehow I'm not surprised.

A partial hominin jawbone has been found in Spain which suggests that humans inhabited Europe at least 500,000 years earlier than previously suspected. The jawbone is 1.3 million years old, which is extraordinary. Check out the excellent images on the BBC version of the story. Maybe, though, later human just liked to carry around pieces of their distant ancestors, eh? Never hear that hypothesis, do you?

A 160-square-mile portion of the Wilkins Ice Shelf in Antarctica collapsed this past week. This article looks at what implications there are here for the local ecology and global ecosystems. Krill seem to be suffering first from the warming because they depend on the ice in their life cycles. Other crustaceans seem to be fluorishing in the warmer waters.

The tuatara in New Zealand, a lizard-like animal long called a "living fossil" for its conservative evolution, is apparently evolving very rapidly now. This is indicated through studies of the accumulation of mutations in its mitochondrial DNA.

I posted images from our latest geological expedition to Israel, if you'd like to see them.


April 7-11

Our Furry Kin (The First Mammals) and The Greening of the Earth: Evolution of Plants
Recommended Reading: W&M pages 310-315, 260-267, 300-302
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #11:

Can it really be the 11th week? Time for plants to make their formal appearance on this website. They've been there for awhile, of course, as a sort of leafy background to tetrapod evolution. The best place to start a general survey of our very distant green cousins is with Berkeley's fossil plants page. Their fossil plants range chart may be especially useful, although we won't be using most of the names given there. By far the most detailed plant website is the University of California on-line paleobotany lab. The diagrams and hierarchical systems of detail here are most impressive. You may want to scan these pages for the beautiful line drawings alone, but the clear and simple text will trap you. If you want professional detail of fossil plant systematics and distribution, click into the homepage of the International Organisation of Palaeobotany. Berkeley's "Deep Green" website on plant diversity is also very impressive. Finally, here's a ginkgo webpage for everything you want to know about this wonderful tree common on our campus (although it is hardly the only "link between the primitive and modern plants").

If you want to take another geology course next semester, I highly recommend Geology 200 (Processes and Concepts of Geology). It is a survey of all the geological subdisciplines, with a tectonic and historical thread through it. You may also consider Geology 260 (Sedimentology & Stratigraphy) taught by your trusty professor.

Here is our memo describing the Final Examination in this course.

Geology in the News:

Who would have guessed that turbidites would be a front-page story on Fox News? A recent study of turbidites off the coast of northern California shows that they were triggered by earthquakes, and that the timing shows that many faults in the Pacific Northwest are "communicating" with each other. (Meaning that they are responding to similar stress fields.)

Here is one of many articles this semester on why geology is turning out to be a very hot major for potential employers. This is especially the case for students who have mastered sedimentology and stratigraphy topics.

Yes, whatever evidence we can get. A human coprolite was found in a cave deposit just over 14,000 years old in Oregon. Its human origin was confirmed by a DNA analysis. (Even at 14,000 years old, I'm still glad I didn't have that job.) This is confirming evidence for a pre-Clovis migration from Asia to North America.

“It’s always difficult to try to interest the public in the rocks themselves,” said Dr Owen. “However, the rocks tell a story about the Earth’s history.” This is in defense of a proposal in Wales to establish a new "Geopark". Of course, we know that rocks are fascinating in themselves, don't we?!

I wrote an editorial for InsideHigherEd.com entitled, "Professors Should Embrace Wikipedia". The fun part is not the essay itself but the many, many comments. I knew Wikipedia annoys some people, and it offends the delicate sensibilities of many academics, but I had no idea the passions ran so hot.

 


April 14-18

Catastrophe: The Cretaceous Mass Extinctions
Recommended Reading: W&M pages 316-317
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #12:

We will finish our plant section on Monday (see previous links) and then spend the rest of the week looking at the incredible story of the Cretaceous Mass Extinctions, sometimes called the "K/T" Extinctions (or "KTX" for the cognoscenti). The "Impact Hypothesis" was developed at the University of California, Berkeley, in 1980 (when I was there as a graduate student, to my great fortune). It seemed absolutely bonkers at the time, but now we see it as one of those intellectual breakthroughs which changed our perspective on the History of Life. Our first website to visit, appropriately, is Berkeley's Cretaceous Extinctions page. You'll love it. It has enough detail to keep us very busy. Note that dinosaurs were apparently cut down in their prime, although there is still much debate about this. (Read that last article very carefully for a little surprise in it!) We will emphasize the Impact Hypothesis in this course because I think it is the one best supported by the evidence. The volcanic hypothesis is still alive, though. Some of its supporters are bitter, claiming that the K/T extinction argument has been thoroughly corrupted by politics; they even ask for a Congressional inquiry! Seems a bit of sour grapes, but read their page. In contrast with the reasonable (more or less), there are many more exotic ideas about dinosaur extinctions, some tallied here and here. And finally, let's not forget that many more organisms than the dinosaurs were affected by the Cretaceous Extinctions.

Here again is the Final Exam Information Sheet. All you need to know about your last test in this course.

Geology in the News:

Here's a Cretaceous snake from Lebanon which has been shown by x-rays to have had two legs. You're not very surprised, though, because you know about vestigial structures and why this would be a prediction from evolutionary theory. Nice to see it, though. And very good to have some positive news out of Lebanon (even if the work was in France).

Here are some very cool new photographs of the Martian moon Phobos. Scientists believe many of the surface features may have formed when material ejected from impacts on Mars later collided with Phobos. The very large impact feature (compared to the size of the moon) is called the Stickney Crater. Must have given this object a wallop.

Speaking of things Martian, did you know NASA has another spacecraft scheduled to land on Mars in about two months? It is called Phoenix, and it will land in a boulder-strewn feature called (optimistically) Green Valley. There may be considerable water ice there. We will learn more about the Martian surface and test these hypotheses about a previous wet interval on the planet.

Evolutionary patterns -- sometimes you can't even make this stuff up. Here is an orchid with a perfume which mimics the odor of a female wasp of a certain species. The goal for the orchid is to lure the male wasps to the flower for pollination. Turns out the flowers are so good at this deception, or the males are so obtuse, that the wasps actually "have sex" with the petals. Good for the flower, but the female wasps must be wondering why they get so little attention! See the video.


April 21-25

Our Cousins at Last: Introduction to Cenozoic Mammals
Recommended Reading: W&M pages 377-394
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #13:

We had our introduction to mammals back in the Triassic. They were ratty little critters then, for the most part, but now that the dinosaurs are gone mammals have become very serious. (Remember, though, that we now know of a raccoon-sized Mesozoic mammal that ate dinosaurs for lunch, albeit small dinosaurs!)

So many mammal groups appeared in the early Cenozoic that we cannot cover them all in this course, or even mention many of them. That diversity dilemma is actually part of the story of the extraordinary adaptive radiation of the mammals, which has been made more complex by recent genetic findings that mammal diversification was not entirely due to the dinosaur extinctions. Note in that story that the three-part division of mammals we see today (monotremes, marsupials and placentals) began in the Cretaceous. This story also introduced me to the "wolf-like cow" Andrewsarchus. Again, the webpages from Berkeley will be highlighted here because they are organized in the most useful ways for us. You will want to look at their short rodents page, and of course make a side visit to the Rat and Mouse Club of America (where one of their ethical principles is that they don't sell their pets to the Snake and Tarantula Club). Now jump WAY up to the proboscidean (elephants, mammoths, mastodons) page, just to delight in the wondrous variety in modern mammals. There are many pages devoted to mammoths, mastodons and other "Ice Age" mammals, including the Pleistocene exhibits at the Russian Paleontological Institute. Carnivores are always interesting, and are in themselves highly diverse. They include wolves, dogs, cats, raccoons, bears, weasels, hyenas, seals, and walruses. A hero to your cat is the ancient sabretooth, highlighted in special exhibits this year at Berkeley and the Illinois State Museum. You can now make another mammal diversity leap to our unlikely cousins the cetaceans (whales and dolphins; here's an Eocene whale recently found in Egypt). The ungulates, or hoofed mammals, are an excellent group to use in a study of evolutionary patterns. The artiodactyls (cloven-hoofed mammals) include the prosaic sheep, goats, camels, pigs, cows, deer, giraffes, and antelopes (and now whales!). Their relatives the perissodactyls ("odd-hoofed" mammals) include rhinos, horses and tapirs today, but they were much more diverse in the past. The evolution of the horse is a classic story, told well at the "Fossil Horses in Cyberspace" site at the Florida Museum of Natural History. Clearly most of this material will be continued into next week.

Here again is the Final Exam Information Sheet. All you need to know about your last test in this course.

Geology in the News:

The 5.2 magnitude earthquake in southern Illinois last week surprised many people, but not, of course, geologists. The 'quake was on an extension of the New Madrid fault system, which is one of the most dangerous in the United States. There was a huge earthquake in the region in 1812 which actually made the Mississippi river run backwards for a short time. Be prepared.

Coral reefs in the western Pacific are about to undergo spectacular spawning during which the individual polyps release billions of eggs and sperm cells into the water at night. This impressive event will be recorded by biologists this year with unprecedented detail.

Looks like we can take an increase in cosmic radiation off the list of factors causing global warming. This idea did not catch on among climate scientists, so it must have been a bit annoying to disprove it, but in the process we learned more about global climate and cosmic rays.

I grew up near the "world's oldest living organisms" which were the bristlecone pines of eastern California. Were. That claim became dodgy with the discovery of various clonal plants which are older. Now the record-holder for the oldest living tree is a 9,550-year-old spruce in the Dalarna province of Sweden. They have the ability to grow new trunks when needed, so the oldest parts are actually below ground.


April 28 - May 2

The Wonders of the Thumb: Primate Evolution
Recommended Reading: W&M pages 397-401
Special Events:
Assignments: (Preparation questions)

Web Resources for Week #14:

During this last week we will concentrate on primate and specifically human evolution. We look closely at our own lineage not just because it is of immediate interest to us, but also because we can directly apply concepts of evolutionary theory to organisms intimately familiar to all of us. The Web has almost as many sites on issues of human evolution as it does on dinosaurs, so most of the addresses I can link you to will provide you with many other connections. Start first with the Institute of Human Origins, now based at Arizona State University. They have an excellent additional website called "becoming human". "A look at modern human origins" is another thorough, updated website, as is the one called "Archaeology.info". The Journal of Human Evolution is online; you can skim the current issue to see what's hot in the field. For still more detail, try the "Dental Microwear Homepage", which has excellent descriptions and images of the microscopic features paleoanthropologists use to suggest the diets of ancient hominids. Try the interactive "skull module" website where you can take pieces of a human skull and manipulate the images on your screen. Very cool. Think evolution here, especially of the mandibles and cranium. "Evolution's Arrow" is a provocative and stimulating online book by John Stewart (not Jon Stewart!) considering the future of human evolution. You should also pay one last visit to the University of California Museum of Paleontology at Berkeley, which has served us so well on this webpage. Their page on primates is not yet complete, but it does have several links to other resources. As you examine these websites, please also keep in mind that the fossil record of hominid evolution has produced numerous competing hypotheses, so you will find many disagreements, even on what seem to be basic observations. (Note, for example, the popular pseudoscience surrounding the "aquatic ape hypothesis".) As an example of the hype and expectations which have dogged the study of human evolution for over a century, here is an excellent TalkOrigins webpage on Piltdown Man.

Here is an excellent and clickable hominid-climate evolution diagram from Lamont-Doherty Earth Observatory (Columbia University) I will show you in class. Remember that we are not using all the hominid names you find on sites like this.

Here again is the Final Exam Information Sheet. All you need to know about your last test in this course.

Geology in the News:

Because of massive droughts lasting thousands of years, humans nearly went extinct 70,000 years ago. Populations in eastern and southern Africa apparently dwindled to less than 2000 total people. This is the conclusion from a massive genetic study of human DNA. Think how closely related we are considering we all share our heritage in these small bands of people who struggled to survive?

Elephants apparently derive from a semi-aquatic ancestor, at least according to the interpretations of fossil teeth of Moeritherium. The oxygen isotopes in the enamel show that their diet was primarily water plants.

Check out photos of new species found in the Carrado Region of Brazil. They include legless lizards, a new mouse opposum, and a horned toad. this is a "biodiversity hotspot" and another indication that there is much more new life out there to find.

A giant squid now thawing out in New Zealand has eyes the size of soccer balls. Largest eyes known today. We think that some giant nautiloids of the Ordovician may have been just as large or larger than the modern giant squids.

 




 May 6 (Tuesday): Final Examination (7:00 p.m.)


 Notes for the History of Life Course

The History of Life course is a broad overview of the evolution and diversification of life on Earth. It is an introduction to science in general and to evolutionary biology and historical geology in particular, but science majors as well as non-scientists will find the material interesting and challenging. This course, in fact, counts toward the major in geology. It is all great fun, especially when you see that the material not only changes every semester, it changes every week. And wait until you see what strange and marvelous events have happened in the History of Life!

We will meet at 8:00 a.m. Monday, Wednesday, and Friday for lectures in Scovel 105. Attendance is required. You are expected to be in the classroom before 8:00 a.m., especially if there is a quiz. If you have trouble getting out of bed for a morning lecture, this is not the course for you.

The grade in this course will be based on two hourly tests, a final examination, and twelve "pop" (unannounced) quizzes. A student not present in class when a quiz is given (even if it is the beginning of the class) will receive a zero for that assignment. Missed quizzes cannot be "made up" for any reason (except a scheduled and conflicting college event), but the lowest two quiz grades will be dropped at the end of the semester. You will also receive a list of preparation questions before each lecture or accompanying some special reading. Occasionally your written answers to these questions will be collected and graded as a quiz. Please note the dates for all the regularly scheduled tests -- these dates will not be changed except under unusual circumstances. In every class at Wooster you should receive a major graded assignment before the drop date. That major assignment in this course is the first test on February 15. I keep all the grades on a spreadsheet so I can quickly calculate your cumulative course average. It is, however, your responsibility to stay informed about your course performance. Just ask me if you have questions about your scores.

This course has been completed by many students, so there are many notebooks out there filled with pages of lecture details. Because ideas, emphases, and even "facts" change rapidly in biology and geology, use old class notes with caution.

It is possible to take this course "S/NC", unless you plan to major in geology. The minimum letter grade for an "S" in this course is C, which is a final average better than 75% on tests and quizzes. I do not encourage the S/NC option -- usually students taking it earn high grades anyway, or they fail with scores below C.

This course is administered under the Code of Academic Integrity, which you should review in your copy of The Scot's Key. Violations of the Code in this course include consulting notes or other student papers during tests and quizzes. My penalties for cheating start with an F in the course and then get worse.

The faculty of the College has recently approved a new policy regarding conflicts between extracurricular and academic events. I agree with it and will simply provide the suggested syllabus statement from the discussion: "The College of Wooster is an academic institution and its fundamental purpose is to stimulate its students to reach the highest standard of intellectual achievement. As an academic institution with this purpose, the College expects students to give the highest priority to their academic responsibilities. When conflicts arise between academic commitments and complementary programs (including athletic, cultural, educational, and volunteer activities), students, faculty, staff, and administrators all share the responsibility of minimizing and resolving them. As a student you have the responsibility to inform the faculty member of potential conflicts as soon as you are aware of them, and to discuss and work with the faculty member to identify alternative ways to fulfill your academic commitments without sacrificing the academic integrity and rigor of the course."

 

Recommended Textbook (not required)

Wicander, R. and J.S. Monroe. 2006. Historical Geology: Evolution of Earth and Life Through Time. (Fifth Edition) Thomson, Brooks/Cole; 440 pages; ISBN 0495012041. [Recommended readings are listed in the lecture outline as "W&M". You do not need to sign up for any online programs, but you are welcome to do this on your own.]

From its title you see that this book covers much more than just the history of life. The reason for such diversity, you will quickly learn, is that life and physical environments are inextricably connected -- life itself is a geological process. I have recommended readings primarily in the origins, evolution and tectonics sections of the textbook, but please don't hesitate to read the more geological portions as well. The publisher has an elaborate textbook companion website with numerous resources including flashcards, animated images, quizzes, online field trips, and more. This site is well worth at least one visit per chapter.

This textbook is not required for the course. The tests and quizzes will be entirely from lecture notes. Most of your reading will be from websites and handouts in class.

 

Grading Format

Testing Date Percentage of Grade Notes
1st Exam February 1 5  20%
2nd Exam April 4  25%
Final Exam May 6, 7:00 p.m.  30%
Quizzes (Pop!) (Unannounced)  25% total Lowest two dropped

 

Teaching Assistant

Elyssa Belding, a junior geology major, is our teaching assistant this semester. Elyssa will also serve as a tutor for this course. She can be most easily reached by e-mail (ebelding09@wooster.edu).

 

Course Instructor

I have an appointment schedule posted outside my office door in Scovel. Please sign up for an appointment if you have any questions or just want to talk. In a large course such as this students often think I am too busy to see them individually unless there is a problem. This is not true. Please visit me if there is anything at all you wish to discuss. The material for this course is too interesting to let it go by as just a series of lectures!

Mark A. Wilson
Scovel 120
Telephone ext. 2247
mwilson@wooster.edu

Pteranodon


Pteranodon by Heinrich Harder (1916)


Science, Evolution, and Creationism ...
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