Wooster Geologists begin the 2011-2012 school year

WOOSTER, OHIO–The cheerful group above is the Wooster Geology Club in our traditional start of the year group photograph. (The image was kindly taken by Danielle Reeder.) We are fewer than usual because an unprecedented number of our geology majors are overseas on off-campus adventures (seven juniors) and our beloved petrologist Meagen Pollock is on a semester research leave. An addition to our crew this year is the man in the upper left with a beard. He is Matt Curren, our new geological technician.

Here you can see happy students in the 8:00 a.m. Invertebrate Paleontology course enjoying their first taste of taxonomic rules and the problem of species. Or maybe they’re grinning because they just learned there is not a quiz this morning?

There are two significant changes in Scovel Hall for this year. We have a new X-Ray Laboratory under the supervision of Dr. Pollock, complete with a “clean room” for wet chemistry. (I know what the alumni are thinking: A clean room in Scovel? But yes, it really is!) We also have fancy new (and wonderfully silent) computer projection systems in our classrooms, as seen below. We are now very far beyond those old 35 mm slide projectors I grew up with.

Our courses have detailed webpages that you are encouraged to visit. You may also want to see our list of Geology Club events, including Independent Study presentations and outside speakers. Finally, you can follow this link to pdf versions of our annual reports, including our report for this past year and summer (see cover below). Patrice Reeder works very hard to produce these high quality documents.

It is going to be another eventful year for the Wooster Geologists. We again thank the generations that have gone before us to build this department, and the alumni and friends who support us so faithfully.

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Wooster’s Fossil of the Week: A trilobite hypostome (Upper Ordovician of southern Ohio)

We had a familiar trilobite last week, so this week we’ll look at a poorly-known part of a trilobite: the hypostome. Above is an incomplete forked, conterminant hypostome of the large trilobite Isotelus. (Isotelus, by the way, is the state fossil of Ohio. Do you know your state fossil?)

Hypostome means “under mouth”. On trilobites it is found underneath the cephalon (head) near what we think was the mouth. They are not common in the fossil record. It is obvious from their color and composition that they are part of a trilobite, but most people don’t know about this little plate on the otherwise soft underside (the ventral side) of the animal. The hypostome is important in some new taxonomic schemes for sorting out the trilobites (Fortey, 1990), and they are useful for interpreting a particular trilobite’s feeding habits (Fortey and Owens, 1999).
Trilobite hypostome forms from Wikipedia (via Obsidian Soul). The small green plates are the hypostomes seen against the gray cephalon above. A – Natant: Hypostome not attached to doublure; aligned with front edge of glabella (shown in red broken lines). B – Conterminant: Hypostome attached to rostral plate of doublure. Aligned with front edge of glabella. C – Impendent: Hypostome attached to rostral plate but not aligned with glabella.

The hypostome of Isotelus is attached to the anterior edge of the skeleton (thus “conterminant”) and has two distally-directed prongs (making it “forked”). Hegna (2010) has recently suggested this hypostome with its unusual shape and terraced outer structure may have been used for grinding food rather than serrating it. Turns out our hypostome has a unique form among the common trilobites!

References:

Fortey, R.A. 1990. Ontogeny, hypostome attachment and trilobite classification. Journal of Paleontology 33: 529-576.

Fortey, R.A. and Owens, R.M. 1999. Feeding habits in trilobites. Palaeontology 42: 429–65.

Hegna, T.A. 2010. The function of forks: Isotelus-type hypostomes and trilobite feeding. Lethaia 43: 411-419.

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Field-based Teaching in Northeastern Minnesota

NORTHEASTERN MINNESOTA – As part of the Cutting Edge workshop on Teaching Mineralogy, Petrology, and Geochemistry, I had the opportunity to participate in a field trip to the Midcontinent Rift System in northeastern Minnesota. You can imagine how exciting this was to an Ohio-based (outcrop-deprived) petrologist! Here’s a quick tour of some of the spectacular stops on the trip:

Keweenawan diabase dike intruding slates and greywackes of the Thomson Formation.

Layering in the Lower Troctolite Zone of the Duluth Complex.

Folding in Archean greywackes of the Lake Vermilion Formation.

 

Multiple generations of folding in the Soudan-type Banded Iron Formation.

Basaltic pillow in the Ely Greenstone with exquisitely preserved glassy textures in the hyaloclastite rims.

Lichen-covered columnar joints in basalt flows of the North Shore Volcanic Group.

A large plagioclase crystal (showing striations) from an anorthosite xenolith.

Learning about the fantastic geology of northeastern Minnesota was only one of our primary goals. The other was to discuss strategies for field-based teaching and learning. There are countless reasons for bringing our students to the field, including two that I consider most important: (1) the field challenges students to exercise their higher-order critical thinking skills (making observations and dealing with complexity); and (2) the field inspires students to learn and be curious of the natural world. The field trip provided an opportunity for “a collection of North America’s greatest geoscience educators”* to share effective teaching ideas for helping students achieve these goals. I’ve compiled a short list of useful tips that I took away from the trip:

  • Enhance the social learning environment – Encourage students to learn something about each other by asking them to line up in order of first name or longitude of their place of birth. Establishing a community enhances peer-to-peer learning, which is a powerful instructional practice in the field.
  • Set and assess goals – For every field trip (and every stop), set specific learning goals, then ask How do we accomplish these goals? How do we know we’ve accomplished these goals? Learning goals and teaching activities will vary with audience and setting. Consider the following example: the learning goal of one particular field trip stop was to observe and describe volcanic features of an outcrop of mafic metavolcanic flows. For the activity, we were provided with an outline of the outcrop and asked to map the distribution of volcanic features from one end to the other. At the end, we compared maps and discussed similarities and differences. The conversation helped us describe the volcanic features we used to define the different units and to determine the stratigraphic “up” direction.
  • Connect the classroom to the field – We’ve all held large maps against the vans to use as visual aids when explaining the geologic setting, but why not laminate poster-sized photomicrographs or phase diagrams to enhance the discussion? By directly applying field observations to concepts they’ve learned in class, students will learn to transfer content knowledge to different settings.
  • Don’t neglect the affective domain – An honorable learning goal is to inspire a sense of awe in students. We certainly had several stops that were breathtakingly beautiful and “reminded all of us why we love geology.” I’m sure most of us can recall a particular field experience that motivated us to pursue geology as a major. Sometimes, it’s the “fun” stops that have the greatest impact.
  • Technology can enhance student learning – One person suggested recording podcasts that students could listen to in the vans between field trip stops. Another person mentioned that smartphones or iPads could be used to take and annotate images of outcrops, which can be loaded onto a wiki later for a collaborative learning project. (The idea probably works equally well for paper photos). On the field trip, we used a portable XRF to measure and compare the compositions of different rock units.

 

The BIF was one of the stunning outcrops where the field trip leaders allowed us to be excited and explore before trying to discuss the geology.

 

Geologists and their toys: playing with the pXRF.

If you have ideas for effective field-based teaching practices or would like to share your experiences, please comment!

*Directly quoted response from field trip leader J. Goodge when a passer-by asked “What is this?”

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Wooster’s Fossil of the Week: A trilobite (Middle Cambrian of Utah)

I’ve avoided having a trilobite as Fossil of the Week because it seems like such a cliché. Everyone knows trilobites, and they are the most common “favorite fossil” (invertebrate, anyway). Plus our best trilobite (seen above) is the most familiar trilobite of all: Elrathia kingii (Meek, 1870). One professional collector — just one guy — said that in 20 years he sold 1.5 million of these.

Still, trilobites are cool. They virtually define the Paleozoic Era, appearing in the Early Cambrian and leaving the stage (with so many others) in the latest Permian. They were arthropods, sharing this very large phylum with insects, spiders, crabs and centipedes. The name “trilobite” means “three lobes” referring to the axial lobe (running down the center along the length of the animal) and the two pleural lobes, one on each side. They  also have three parts the other way: a head, thorax and pygidium (the tail end).

Elrathia kingii is a ptychopariid trilobite found in extraordinary numbers in Middle Cambrian dark shales and limestones. There is a geological story here, two of them, in fact. One reason they are so common is that their populations were commonly buried by sediment stirred up in massive storms (Brett et al., 2009). They are among the only fossils found in organic-rich dark sediments because they lived in the harsh “exaerobic zone” at the very minimum of oxygen needed for animal life (Gaines and Droser, 2003). They apparently were the first large invertebrates to exploit this marginal environment.
Elrathia kingii gives us the opportunity to meet a pioneering American paleontologist: Fielding Bradford Meek (1817-1876). He originally described this species in 1870, calling it Conocoryphe kingii (see above). Paleontologists are quite familiar with the name “Meek” following a fossil species because he described hundreds of them. Meek was a native of Madison, Indiana, a place where Ordovician fossils are abundant and easily collected. He was apparently an unsuccessful businessman so he jumped at a chance in 1848 to work for the U.S. government surveying the geology of Iowa. Meek was good at this job and soon was working with James Hall in New York, the country’s premier paleontologist. Meek was eventually based in Washington, D.C., with the United States geological and geographical surveys. After many accomplishments in government service, he died of tuberculosis in 1876 (White, 1896).

Fielding Bradford Meek

References:

Brett C.E., Allison P.A., DeSantis M.K., Liddell W.D. and Kramer A. 2009. Sequence stratigraphy, cyclic facies, and lagerstätten in the Middle Cambrian Wheeler and Marjum Formations, Great Basin, Utah. Palaeogeography, Palaeoclimatology, Palaeoecology 277: 9-33.

Gaines, R.R. and Droser, M.L. 2003. Paleoecology of the familiar trilobite Elrathia kingii: An early exaerobic zone inhabitant. Geology 31: 941–944.

White, C.A. 1896. Memoir of Fielding Bradford Meek, 1817-1876. Biographical Memoirs, National Academy of Sciences, p. 75-91.

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Teaching Mineralogy, Petrology, and Geochemistry

MINNEAPOLIS, MN – If you haven’t been following my twitter feed (http://twitter.com/meagenpollock), you may not know that I’ve been at the 2011 Cutting Edge Workshop on Teaching Mineralogy, Petrology, and Geochemistry (twitter hashtag #sercMPG). Expert educators have gathered to discuss teaching strategies, develop course materials, and exchange ideas about issues in MPG. Fortunately, the Cutting Edge runs several workshops across the geoscience disciplines (look for the updates in September), which have generated an invaluable collection of teaching resources. You’ll be able to find all of the materials from this workshop on the web and we’ll be adding more teaching activities soon after the workshop ends. Here’s a quick (and incomplete) list of resources that I’ve discovered:

Please comment here or add to the Cutting Edge collection if you have useful MPG teaching resources!

According to the Cutting Edge: "Core of Ely Greenstone outside Pillsbury Hall, home of the Geology & Geophysics Department at the University of Minnesota. Metamorphosed Archean basalt pillows are visible in the core, which is approximately 2 meters tall. Photo by Sharon Kressler." Aka: What I want for my next birthday!

 

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Using the iPad in museum work

COLUMBUS, OHIO–Earlier this summer my colleagues and I had blog posts describing how we use our iPads in geological fieldwork (with examples from the limestones of Estonia to the basalts of Iceland). Today I used my iPad2 during work in the collections of the Orton Geological Museum at The Ohio State University.

The simple camera utility built into the iPad2 makes recording quick images of specimens in their drawers and trays very easy. The LED backlighting makes the large image on the screen brighter than the actual view, which you can see in the photo above. Combine this with the light weight of the computer and it is actually easier to use the iPad2 for these images than a standard digital camera. The quality of the iPad2 image is not as good as that from a camera (with flash or auxiliary lighting), but we’re just collecting initial views and labels with this process (see below).

As with the images collecting during fieldwork, I can easily annotate the museum photographs with a program like Sketchbook Express. (Circling features for later detailed camera photography is what I do most often — museum staff typically don’t like us drawing on the specimens themselves!) The Boxwave Stylus remains my favorite drawing tool on the iPad2.

The iPad2 is also the most convenient repository of scientific papers I have ever used. It can store thousands of pdfs for quick referencing. The luminous screen makes reading them in the typical dingy light of museum collections easy, and images and text can be expanded for more visual detail. (Try that with paper!) A laptop certainly does these same things, but far more awkwardly while hunched over a museum drawer. The program I use for pdfs is PDFReader Pro (with pdfs transferred through Dropbox), but my friend Bill Ausich at The Ohio State University showed me that iBooks is just as easy to use.

I like to store specimen images from other sources to compare to the fossils in the drawers before me — making identifications this quickly helps me decide which specimens to borrow for later work. I can store the images as jpg files in the iPad2 Photo library or view them as pdfs in PDFReader Pro.

If you can get a wireless connection in the museum (often quirky in old buildings), searching for the meaning of strange stratigraphic terms and archaic species names is obviously of great value. Again, tapping on the iPad2 held in one hand while looking at the specimens themselves is a qualitatively different experience than returning to the laptop in some dark corner. (I could never have guessed that there would be a computer more convenient than my trusty MacBook Pro.)

In summary, the iPad2 has quickly become indispensable for my paleontological work in museums.

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Keck Mission Accomplished

WOOSTER, OH – After a month of hard work, the Iceland Keck group parted ways on Saturday. We arrived in Wooster immediately after returning from Iceland and put in a solid week of work in the lab, preparing our samples for thin sections and XRF analyses. In one week, the students produced over 120 thin section billets, powders, and pressed pellets, and almost as many glass beads. Even though the work was tedious and the hours were long, I think we’re all glad that we’ll have data at the start of the school year. Well done, team!

A dessicator full of pressed pellets ready to analyze on the XRF.

 

Challenges of lab work. We tracked the number of samples that were prepared. This student prepped 20 pressed pellets "of varying degrees of brilliance + some epic failures."

Katharine works her magic on the scale.

Erica grinds the saw marks off of her sample.

Nina presses a brilliant pellet.

Thad oxidizes his samples in the muffle furnace.

Emily celebrates a glass bead that hasn't cracked.

Brennan and Katie troubleshoot the GIS file.

Of course, our work isn’t complete. Once we have the chemistry and thin section observations, we can put the data into the context of the mapped field relationships to understand the volcanic history of one of the oldest central volcanoes in Iceland. We’ll have much to present at the Keck Symposium in the spring and are already looking forward to our reunion.

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Wooster’s Fossils of the Week: barnacle borings (Middle Jurassic of Israel)

Tiny little trace fossils this week in a Jurassic crinoid stem from the Matmor Formation of the Negev Desert. They are borings produced by barnacles, which are sedentary crustaceans more typically found in conical shells of their own making. These barnacles are still around today, so we know quite a bit about their biology. (More on how in a minute.) These acrothoracican barnacles drill into shells head-down and then kick their legs up through the opening to filter seawater for food. They’ve been doing it since the Devonian Period (Seilacher, 1969; Lambers and Boekschoten, 1986).

This particular trace fossil is Rogerella elliptica Codez & Saint-Seine, 1958. It is part of a diverse set of borings in the Matmor Formation (Callovian) of Hamakhtesh Hagadol, Israel, recently described in Wilson et al. (2010).

We know so much about boring barnacles because Charles Darwin himself took an almost obsessive interest in them early in his scientific career. While on his famous voyage in the HMS Beagle, Darwin noticed small holes in a conch shell, and he dug out from one of them a curious little animal shown in the diagram below.


Cryptophialus Darwin, 1854

He called it “Mr. Arthrobalanus” in his zoological notes. He figured out early that it was a barnacle, but he was astonished at how different it was from others of its kind. He later gave it a scientific name (Cryptophialus Darwin, 1854) and took on the problem of barnacle systematics and ecology. Eight years and four volumes later his young son would ask one of his friends, “Where does your father do his barnacles?” The diversity of barnacles played a large role in Darwin’s intellectual development and, consequently, his revolutionary ideas about evolution (Deutsch, 2009).

Burrowing barnacle diagram from an 1876 issue of Popular Science Monthly.

References:

Codez, J. and Saint-Seine, R. de. 1958. Révision des cirripedes acrothoracique fossiles. Bull. Soc. géol. France 7: 699-719.

Darwin, C.R. 1854. Living Cirripedia, The Balanidae, (or sessile cirripedes); the Verrucidae. Vol. 2. London: The Ray Society.

Deutsch, J.S. 2009. Darwin and the cirripedes: Insights and dreadful blunders. Integrative Zoology 4: 316–322.

Lambers, P. and Boekschoten, G.J. 1986. On fossil and recent borings produced by acrothoracic cirripeds. Geologie en Mijnbouw 65: 257–268.

Seilacher, A. 1969. Paleoecology of boring barnacles. American Zoologist 9: 705–719.

Wilson, M.A., Feldman, H.R. and Krivicich, E.B. 2010. Bioerosion in an equatorial Middle Jurassic coral-sponge reef community (Callovian, Matmor Formation, southern Israel). Palaeogeography, Palaeoclimatology, Palaeoecology 289: 93-101.

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A Keck Adventure at 66 North

West Fjords, Iceland – We’re happy to report that the 2011 Iceland Keck crew has safely completed a productive field season. Nearly two weeks ago, a boat dropped us off in Hornstrandir, a nature preserve that encompasses most of the northern portion of the West Fjords. Our field area centered around Hrafnsfjordur, or Raven Fjord, in the southern extent of Hornstrandir. We had no idea that Hrafnsfjordur was a popular destination; it’s one of the primary drop-off and pick-up points for backpackers in the region. We must have seen at least half a dozen hikers during our stay. Hiking trails snake their way around the fjord and over the passes, which was fortunate for us since we had to access all of our field areas on foot.

A very still day in Hrafnsfjordur.

After a couple of days of recon hiking as a group, the students selected their projects and went to work. Most students chose to map a portion of the fjord, although one student focused on mapping and sampling dikes. Students worked in teams of two, each team being assisted by a faculty member.

A very sunny day in Hornstrandir.

Field work was challenging. Like our Alaskan colleagues, we had dramatic stream crossings, treks across snow, and hikes up steep terrain. Although we never saw a bear, we spotted an arctic fox in the distance. Thankfully, the fox wasn’t interested in our food. Dehydrated meals at the end of a long field day never tasted so good!

Coast guard performing drills outside our hostel in Isafjordur.

The weather was mostly good, by Iceland standards. It seems as if we were constantly confronted with either bugs, wind, or rain, but always just one at a time. Whenever Emily worked in her area, though, the sun would shine!

Hiking up snow to reach the peak.

We took a chartered boat back to Isafjordur on Wednesday and spent one last day in the field mapping a local mountain called Sauratindur. Now that we’re finished with field work and have returned to civilization, we realize how thankful we are for hot showers and soft mattresses. Still, there are some things that we’re already missing: the view from our tents, the sound of the waterfall (especially at night), the soft moss, our own private fjord, the hot cocoa, our special treat at the end of each day, and the freshness of the air.

Our Keck adventure in Hrafnsfjordur, in Hornstrandir.

Tomorrow, we start our long journey back to the states (via Reykjavik). We’re eager to get back to Wooster to start processing our samples. Hrafnsfjordur offered us an amazing amount of what we think are intermediate lava flows, which would be unique for Iceland. Dominated by basalt with local regions of rhyolite around central volcanoes, intermediate lavas are relatively sparse. Our field mapping, thin section observations, and geochemical analyses should yield some insights into the formation of Hrafnsfjordur’s central volcano. Stay tuned!

Panorama from the top of Manafell in Hrafnsfjordur.

Students playing a game of rock while waiting on the boat.

Textbook hanging valley in Isafjordur.

The boat that came to pick us up- one trip for gear and rocks!

The view from my tent in Hranfsfjordur, Keck.

Familiar scene for geo types- hiking up waterfall cuts for good exposure.

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Wooster’s Fossil of the Week: An edrioasteroid (Upper Ordovician of Kentucky)

This week’s fossil appeared previously in this blog when we discussed hiatus concretions and their fossil fauna. It is one of my favorites for both how we found it (see the entry linked above) and the way it introduced me to hard substrate fossils (it was my first). The edrioasteroid is the circular fossil in the center. Above it is a branching cyclostome bryozoan that will be the subject of another story someday. These fossils were found in the Kope Formation (Cincinnatian Group) of the Upper Ordovician in northern Kentucky, making them about 450 million years old.

Edrioasteroids (“seated stars”) were echinoderms (spiny-skinned animals) that lived from the Cambrian through the Permian periods (Sumrall, 2009). Their living relatives today include sea stars, sea urchins, sand dollars and crinoids. Edrioasteroids have a flattened disk-like body called a theca covered with plates of calcite. They attached themselves to hard substrates like shells, hardgrounds or cobbles (as in the photo above). On the upper surface of the theca are ambulacra extending outward from a central mouth. The anus is a little circular set of plates between two of the ambulacra. The ambulacra themselves had tiny little tube feet that extended upwards into the seawater  for filter-feeding suspended organic matter.

The fossil above, also represented in the diagram below, is Cystaster stellatus (Hall, 1866). It is a small edrioasteroid, as the group goes, and is characterized by straight, wide ambulacra.

(Image from the Cincinnati Dry Dredgers’ wonderful website.)

(Image from the public domain Encyclopaedia Britannica, 11th Edition.)

Edrioasteroids are favorite fossils for collectors. I learned this when I published a paper on the fauna that included the fossils above (Wilson, 1985) and later the outcrop was pillaged — not a single edrioasteroid remains there from the hundreds originally found.

References:

Sumrall, C.D. 2009. First definite record of Permian edrioasteroids; Neoisorophusella maslennikovi n. sp. from the Kungurian of northeast Russia. Journal of Paleontology 83: 990-993.

Wilson, M.A. 1985. Disturbance and ecologic succession in an Upper Ordovician cobble-dwelling hardground fauna. Science 228: 575-577.

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