Expanding Your Horizons in Geology

Wooster, OH – The Wooster X-ray Lab hosted girls from the Expanding Your Horizons program, a series of workshops aimed at encouraging young women to pursue careers in the sciences. The geology workshop focused on minerals and their wide variety of uses. One popular use of minerals is in beaded jewelry.

These colorful beads are made of minerals.

These colorful beads are actually polished pieces of minerals.

Our goal was to figure out which minerals each bead represented. To do this, we used the X-ray Diffractometer (XRD).  The XRD zaps the minerals with X-rays, which get reflected off of the atomic layers in the minerals, giving us information about their structures. Each mineral has a unique set of reflections, sort of like a fingerprint, which allows us to identify the mineral.

One of the girls prepares a sample for the XRD.

One of the girls prepares a sample for the XRD.

While we were waiting for the samples to run, the girls made bracelets out of the beads.

While we were waiting for the samples to run, the girls made bracelets out of the beads.

Someone made a bracelet that said, "Science Rocks!"

Someone made a bracelet that said, “Science Rocks!” We love the geology pun.

By the end of the workshop, we learned that three of our beads were actually varieties of quartz: Tiger’s Eye Quartz, Amethyst, and Jasper. Our dark blue bead was Sodalite. Maybe the most surprising result was the bead that looked like Turquoise. It was actually Calcite!  Tricky, tricky!

 

 

 

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Virtual Cascades Volcano Observatory in Wooster

Wooster, OH – We hosted a virtual visitor in today’s GeoClub seminar. Dave Ramsay, a geologist from the Cascades Volcano Observatory, connected with us via the web to tell us about the geology of Crater Lake.

Shelley Judge and Dave Ramsey bumped into eachother at the conference on Volcanism in the American Southwest. Both are alumni of the same undergraduate geology program!

Shelley Judge and Dave Ramsey bumped into eachother at the conference on Volcanism in the American Southwest. Both are alumni of the same undergraduate geology program!

Dave and his colleagues have done fantastic work mapping the floor of Crater Lake. Crater Lake formed from the explosive eruption of Mount Mazama about 7700 years ago. On most geologic maps, Crater Lake is a blue body of water. But Dave and his colleagues used multibeam swath echo sounders and a human occupied submersible to map the geology of the lake floor.

Map of Crater Lake showing features of interest on the lake floor. Klimasauskas, E., Bacon, C., and Alexander, J., 2002, Mount Mazama and Crater Lake: Growth and Destruction of a Cascade Volcano: U.S. Geological Survey Fact Sheet 092-02.

Dave took us on a fly-through tour of the geology and told us stories about how many of the geologic features developed. He and his colleagues found that Wizard Island is much bigger than we may have expected, and that it erupted both under and above water while Merriam Cone erupted exclusively under water.

Snapshot of the geology of the floor of Crater Lake.  Here, Wizard Island (gray peak) extends below the water (green). (Photo Credit: David Ramsey).

Snapshot of the geology of the floor of Crater Lake. Here, Wizard Island (gray peak) extends below the water (green). (Photo Credit: David Ramsey).

Many thanks to Dave for talking to us first thing this morning (west coast time) and for giving such an engaging and entertaining seminar.

 

 

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Wooster’s Fossil of the Week: A camerate crinoid from the Lower Carboniferous of north-central Ohio

Cusacrinus_daphne033013Visitors often bring rocks and fossils to the Geology Department for identification. We love to solve the puzzles (or at least make the attempt), and our new friends appreciate names and ages for their treasures. (Usually. We’ve disappointed more than a few finders of “meteorites”.) Last week a home-schooling group came in from nearby Ashland with a tray of stones they found in a stream bed eroding an exposure of the Lower Carboniferous (Kinderhookian) Meadville Shale Member of the Cuyahoga Formation. One of the objects was the spectacular fossil shown above.

This is a calyx and the attached arms (essentially the “head”) of a camerate crinoid known as Cusacrinus daphne (Hall, 1863). (Our friend Bill Ausich of Ohio State University provided the identification — these crinoids are his speciality.) It is preserved as an external mold, meaning that the actual skeleton was covered in sediment (or in this case a concretion) and then dissolved away, leaving a cavity showing a mold of its exterior details. It is a rare fossil to find in our part of the world.

CrinoidCalyx033013Above is a close-up of the calyx of Cusacrinus daphne (Hall, 1863). Note the radiating ridges on the exteriors of each thecal plate. They are characteristic of this species.

CrinoidArms033013These are some of the arms of the crinoid. They are complex because each arm is lined with tiny branches called pinnules, making feather-like extensions for filter-feeding.

Thank you to our new Ashland friends for sharing such a beauty with us!

References:

Ausich, W.I. and Roeser, E.W. 2012. Camerate and disparid crinoids from the Late Kinderhookian Meadville Shale, Cuyahoga Formation of Ohio. Journal of Paleontology 86: 488-507.

Kammer, T.W. and Roeser, E.W. 2012. Cladid crinoids from the Late Kinderhookian Meadville Shale, Cuyahoga Formation of Ohio. Journal of Paleontology 86: 470-487.

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Wooster’s Fossil of the Week: A pretty little fish from the Eocene of Wyoming

Knightia_eocaena_033013_585Most people have seen this fossil fish type. Geologists, in fact, have probably seen Knightia eocaena Jordan, 1907, thousands of times. It is present in nearly every gift shop that sells fossils, usually as small plaques or glued to refrigerator magnets. It is the state fossil of Wyoming and, by all accounts, the most numerous fossil fish in the world. In fact, it is likely the most common vertebrate fossil ever. It is thus no surprise that Wooster has dozens of specimens, most of them donated by students and alumni.

Knightia lived in freshwater lakes throughout western North America during the Eocene. It is closely related to herring and sardines, and almost certainly had similar life habits. We know that it lived in large schools, and we suspect it had a diet of phytoplankton and insect larvae. It was low on the ecological food chain, just like its modern cousins, and so was an important food source for all sorts of larger fish, reptiles, birds and mammals.
MeagensFish585We tend to see most often beautifully preserved, complete Knightia specimens like the one at the top of the page. This is because if a fossil is very common, collectors can afford to keep only the best specimens. It is fun, though, to see what the average Knightia looks like in the fossil record. Above is a specimen collected by our petrologist Meagen Pollock from an outcrop in Wyoming. Note that the fish are contorted and often overlapping — specimens that are usually discarded by collectors. This slab shows better that these fossils occur in vast, complicated, messy death assemblages, probably because of volcanic ash falls or quick changes in lake chemistry.
Knightia_BW_TamuraThis is a digital reconstruction of Knightia (© N. Tamura). Note the deeply forked tail and flattened top of the head.

Dsjordan_wikipediaKnightia was named in 1907 by the accomplished and very problematic David Starr Jordan (1851-1931). Jordan was a well known fish expert, having been inspired by the iconic ichthyologist Louis Agassiz himself. He taught at several colleges and universities, eventually serving as president of Indiana University (at 34, the youngest university president at the time) and as the first president of Stanford University. He was a very successful university president, especially in the first years of Stanford.

But, but … David Starr Jordan was also a eugenicist, believing in compulsory sterilization of the “unfit”. On the bright side (if there is one here), he opposed war because it tended to kill the most fit members of society. Jordan also shockingly covered up the apparent murder of Jane Stanford, co-founder of the university, in 1905. Jordan does not look good at all in that story, most of which was sorted out only about ten years ago. Who would have guessed that a murder mystery could lurk in the taxonomic history of these pretty little fish?

References:

Grande, L. 1982. A revision of the fossil genus Knightia, with a description of a new genus from the Green River Formation (Teleostei, Clupeidae). American Museum Novitates 2731: 1-22.

Jordan, D.S. 1907. The fossil fishes of California; with supplementary notes on other species of extinct fishes. Bulletin, Department of Geology, University of California 5:136.

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The field trip scout

MeadvilleLodi033013WOOSTER, OHIO–One of the early spring pleasures of a geologist in the Upper Midwest is finally getting outside and scouting the field trips for the semester. Today we had bright sun and temperatures in the 50s (I know — I’m settling) so I went out to plan the late April field trip for my sedimentology and stratigraphy class. The sites I’ve been using in the last few years have become too overgrown, so it is time to find new projects in new places. Since the delightfully underbrush-free Mojave Desert is too far away, I’m looking at places in northeastern Ohio. It was a fun day.

Above is an outcrop of the Meadville Shale Member of the Cuyahoga Formation (Lower Carboniferous, late Kinderhookian) exposed in the Lodi Community Park about 20 miles north of Wooster. A tributary of the Black River (the East Fork Black River) flows through a small valley, exposing the shale in its cutbanks. I’m a bit partial to this location because from here a fellow Wooster student found a trilobite that became the basis of my first scientific publication. The unit here is moderately fossiliferous and contains numerous rock types besides shale. It will make a fine place for students to measure and describe stratigraphic sections next month. It certainly was a beautiful place to spend a sunny Saturday morning.

TurkeyVulture033013There were many turkey vultures (Cathartes aura) perched in the still-leafless trees in northern Wayne and southern Medina Counties. Here’s one keeping an eye on me. Turkey vultures are a sign in Ohio that spring really is coming (even if it is supposed to snow tomorrow morning!).

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Dr. Michael Mann visits Wooster

MichaelMann032713WOOSTER, OHIO–We were honored this week when Dr. Michael E. Mann, one of the world’s foremost climate-change experts and a leader in the efforts to educate the public about anthropogenic effects on the atmosphere, came to Wooster as part of our Richard G. Osgood, Jr., Memorial Lecture series. He gave a public lecture in the nearly-full Gault Recital Hall Wednesday evening (“The Hockey Stick and the Climate Wars: Dispatches from the Front Lines”), and then a Geology Club lecture the next day in Scovel (“The Past as Prologue: Learning from the Climate Changes in Past Centuries”). Students, faculty and staff of the Geology Department also had a wonderfully informative dinner with him in the Wooster Inn.

Michael Mann is very well known in the diverse community that studies climate change in the past, present and future. He was the senior author of a pivotal article in the Intergovernmental Panel on Climate Change (IPCC) Third Scientific Assessment Report in 2001. It set the direction for more than a decade of later climate research. He has written dozens of other papers and two books on climate change. He has received numerous awards, most recently the Hans Oeschger Medal of the European Geosciences Union.

The public Osgood lecture Dr. Mann presented on Wednesday was centered on his latest book. He described the recent scientific history of climate change research and then how he became an “accidental public figure” through the famous “Climategate” theft and publication of private email messages. His stories of attempted congressional interference in his work and that of other climate scientists were astonishing, representing what he calls “the scientization of politics” (where science — or pseudoscience — is used as a political tool).

The image at the top of the page is Dr. Mann near the end of his Osgood Lecture. The image on the screen is of his daughter enjoying a moment in the polar bear pool at the Pittsburgh Zoo and PPG Aquarium. He fears that someday such animals will be found only in zoos because humans “melted their Arctic environment.” Numerous questions and conversations followed.
MannLecture032813Dr. Mann gave a Geology Club presentation this morning in Scovel Hall on some of his scientific work (shown above). He talked about using proxies to model historical climate change and then predict future climate.
WilesMann032813For me one of the best moments was his conversation with Greg Wiles in our dendrochronology lab (above). It was great fun to see how the work of Wooster Geologists is part of the unfolding grand story of what factors control our climate, and why such research is critical in our efforts to cope with future changes.

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Wooster’s Fossil of the Week: A grazed oyster from the Middle Jurassic of Gloucestershire, England

Praeexogyra_acuminata_585This small oyster is not in itself unusual. In fact, it is one of the most common fossils in the Jurassic of western Europe: Praeexogyra acuminata (Sowerby, 1816). It may be better known by its older name: Ostrea acuminata. Local collectors call it the “sickle oyster” because of its curved shape. This specimen is from the Sharp’s Hill Formation (Middle Bathonian) exposed in the Snowshill Quarry near Moreton-in-Marsh, Gloucestershire, England. I collected it on my first trip to England in 1985.
Praeexogyra_acuminata_closerWhat attracted me to this particular shell can be seen in the above close-up: lots of little straight lines incised across its outer surface (along with a serpulid worm tube). The lines were scraped by the Aristotle’s Lantern of one or more regular echinoids (sea urchins). This is the trace fossil Gnathichnus pentax Bromley, 1975. We met this fossil last month cut into a Cretaceous oyster from Israel. One or more echinoids grazed over this Jurassic oyster, probably consuming algae and other organic materials.

Praeexogyra acuminata was an epifaunal filter-feeder, meaning it lived on the substrate sucking in seawater and sorting from it organic material for food. During the Middle Jurassic these oysters were so common that their shells formed thick deposits. It is possible that some deposits rich in these shells were formed in brackish waters rather than under fully marine conditions.

Ostrea acuminata was named by by the enthusiastic English natural historian James Sowerby (1757-1822). We met him earlier as the author of a Cretaceous bivalve genus.

References:

Bernard-Dumanois, A. and Delance, J-H. 1983. Microperforations par algues et champignons sur les coquilles des «Marnes à Ostrea acuminata (Bajocien supérieur) de Bourgogne (France), relations avec le milieu et utilisation paléobathymétrique. Geobios 16: 419-429.

Bernard-Dumanois, A. and Rat, P. 1983. Etagement des milieux sédimentaires marins. Paléoécologie des Huîtres dans les “Marnes à Ostrea acuminata” du Bajocien de Bourgogne (France). Comptes rendus de l’Académie des sciences Paris 296: 733-737.

Hudson, J.D. and Palmer, T.J. 1976. A euryhaline oyster from the Middle Jurassic and the origin of true oysters. Palaeontology 19: 79-93.

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Wooster Geologist at Valley Forge, Pennsylvania

ValleyForgeHuts032013BRYN MAWR, PENNSYLVANIA–While visiting my friends and colleagues Katherine and Pedro Marenco at Bryn Mawr College, I visited the nearby Valley Forge National Historical Park. Everyone will remember, of course that this is the place outside Philadelphia that the Continental Army made its rough winter quarters in 1777-1778. The huts above are reconstructions of the soldiers’ quarters on the windy and cold fields. Commander-in-Chief George Washington chose this place because it was easily defensible, had plenty of timber for construction and fuel, and was close enough to British-occupied Philadelphia to keep an eye on the enemy — yet not so close to be likely attacked.

LedgerOutcrop032013

As a geologist, of course, I also looked for the rocky bones beneath the landscape. They were easily found in the above cliff near the main parking area. This is the Ledger Dolomite, a Cambrian unit found throughout this part of eastern Pennsylvania.

LedgerDolomite032013The Ledger Dolomite here is distinguished by these fine laminations visible on its weathered cross-sections. These are apparently stromatolites: laminar structures built by bacterial mats. We’ve met Cambrian stromatolites before in this blog.

Smilodon_gracilisI was surprised to learn that there is also a significant middle Pleistocene fossil deposit in Valley Forge called the Port Kennedy Bone Cave. This is a sinkhole deposit within the Ledger Dolomite. A particularly large sinkhole apparently trapped a variety of animals, including the gracile sabre-tooth Smilodon gracilis, the skull of which is on display in the Valley Forge Historical Park visitor center. S. gracilis was the smallest and earliest member of its genus. The Port Kennedy Bone Cave was one of the first fossil assemblages that the famous paleontologist Edward Drinker Cope studied. The location was lost to science until its rediscovery in 2005.

ValleyForgeCannon032013This is the requisite cannon image, even though no battle was fought here. It is nevertheless a dramatic place for the privations the soldiers suffered during the darkest days of the Revolutionary War. It is hard to imagine the conditions in 1777-1778 now since highways and casinos surround the old encampment.

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Wooster’s Fossil of the Week: Cast of a lower jawbone of the largest ape ever (Pleistocene, southern China)

Gigantopithecus_blacki_mandible_010112The above is one of my favorite “fossils”, a commercially-available cast of the lower jawbone of Gigantopithecus blacki, a giant extinct ape. It was produced from an actual Pleistocene fossil found in a cave near Liucheng, Guangxi, in southern China. I like it especially because it is sometimes associated with the mythical “Bigfoot”.

Gigantopithecus blacki was the largest ape that ever lived: up to three meters tall and weighing over 500 kilograms. (G. blacki is known only from teeth and mandibles such as that shown above, so these size estimates are based on scaling.) It was a contemporary with early versions of our own species, which must have led to a few astounding encounters for our ancestors. G. blacki was two or three times heavier than the largest gorillas today.

Gigantopithecus blacki appears to have lived in bamboo forests. Striations on its teeth, and the occasional phytolith stuck in the enamel, shows that this species was a vegetarian. It may have even had a lifestyle much like today’s pandas.

The molars of Gigantopithecus blacki look surprisingly like ours with their multiple cusps and broad surfaces. This is the result of convergent evolution and not an indication of a recent common ancestry. (They are analogous features, not homologous.) G. blacki is now classified in the Subfamily Ponginae with their cousins the orangutans.

What is most fun about Gigantopithecus these days is its association with the “Bigfoot” illusion. Look at how seriously the people at the “Bigfoot Field Researchers Organization” take the possible connection of Gigantopithecus and Bigfoot. Despite their objections, we really can wonder why we’ve never found evidence of this giant ape in North America, including bones, teeth, legitimate footprints or real photographs. A living three-meter tall ape is a bit difficult for science to have missed! (Unless, of course, Bigfoot has supernatural powers.)

References:

Coichon, R. 1991. The ape that was – Asian fossils reveal humanity’s giant cousin. Natural History 100: 54–62.

Ciochon, R., et al. 1996. Dated co-occurrence of Homo erectus and Gigantopithecus from Tham Khuyen Cave, Vietnam. Proceedings of the National Academy of Sciences of the United States of America 93: 3016–3020.

Jin, C., et al. 2009. A newly discovered Gigantopithecus fauna from Sanhe Cave, Chongzuo, Guangxi, South China. Chinese Science Bulletin 54: 788-797.

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Last day in the Mojave Desert for Wooster Geologists … this year

RedRocks031513LAS VEGAS, NEVADA–We left the fine people at the Desert Studies Center in Zzyzx in the morning and drove in an all-too-irregular way through Las Vegas (sorry about that, other drivers!) to the spectacular Red Rocks National Conservation Area northwest of the city. Here we see a Paleozoic section thrust from the west over the white and red rocks of the Aztec Sandstone (Lower Jurassic). The view above is looking directly west from the visitor center. I don’t know all the names of these peaks, but I do recognize Mount Wilson on the left. (I did my dissertation in the Carboniferous rocks exposed in the background, but I don’t think they named the mountain after me.)

Our students, faculty and staff scattered for a couple of hours in this park on yet again a very pleasant day. Many of them climbed the sandstone cliffs, no doubt impressed by the large foresets showing that these sediments were deposited in massive dunes blown in from the east.

RedRocksVisitorCenter031513The redesigned visitor center at Red Rocks is excellent. Above is a view of part of the outside portion that takes advantage of the sun’s angle and cooling breezes. It includes a desert tortoise enclosure where we saw three of these endangered animals. This complex is so attractive and efficient that Yoav Avni took many photographs so that he could show Israeli planners some new ideas for their public displays.

At noon we drove back into Las Vegas and the open jaws of the McCarran Airport Complex. We turned in all four vans with no problems, got our boarding passes for our various destinations, and now are simply waiting in the airport for our flights out. An excellent and enjoyable trip in all respects. Here’s to Jason and Rob at the Desert Studies Center for their friendly and efficient management, to the rangers of the National Park Service for their helpful advice, to the faculty and staff leaders and drivers (so many miles!), and finally to the students who could not have been better ambassadors for Wooster Geology. Their enthusiasm and good humor is what makes these trips so special. We will return!

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