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Wooster’s Fossils of the Week: Chaetetids from the Upper Carboniferous of Liaoning Province, North China

September 22nd, 2017

1 Benxi chaetetid 2a 585Three years ago I had a short and painful trip to China to meet my new colleague and friend Yongli Zhang (Department of Geology, Northeastern University, Shenyang). The China part was great; the pain was from an unfortunately-timed kidney stone I brought with me. Nevertheless, I got to meet my new colleagues and we continued on a project involving hard substrates in the Upper Carboniferous of north China. Above is one of our most important fossils, a chaetetid demosponge from the Benxi Formation (Moscovian) exposed in the Benxi area of eastern Liaoning Province. We are looking at a polished cross-section through a limestone showing the tubular, encrusting chaetetids. This month the paper on these fossils has at last appeared.
2 Chaetetid Benxi Formation (Moscovian) Benxi Liaoning China 585This closer view shows two chaetetids. The bottom specimen grew first, was covered by calcareous sediment, and then the system was cemented on the seafloor. After a bit of erosion (marked by the gray surface cutting across the image two-thirds of the way up), another chaetetid grew across what was then a hardground that partially truncated the first chaetetid. This little scenario was repeated numerous times in this limestone, producing a kind of bindstone with the chaetetids as a common framework builder.
3 Chaetetid Benxi cross-section 585Here is the closest view of the chaetetids, showing the tubules running vertically, each with a series of small diaphragms as horizontal floors.

Last week’s fossil was a chaetetid, introducing the group. They are hyper-calcified demosponges, and the classification of the fossil forms is still not clear. Their value for paleoecological studies, though, is clear. This particular chaetetid from the Benxi Formation preferred a shallow, warm, carbonate environment, and it was part of a diverse community of corals, fusulinids, foraminiferans, brachiopods, crinoids, bryozoans, gastropods, and algae. Such hard substrate communities are not well known in the Carboniferous, and this is one of the best.

References:

Gong, E.P, Zhang, Y.L., Guan, C.Q. and Chen, X.H. 2012. The Carboniferous reefs in China. Journal of Palaeogeography 1: 27-42.

West, R.R. 2011a. Part E, Revised, Volume 4, Chapter 2A: Introduction to the fossil hypercalcified chaetetid-type Porifera (Demospongiae). Treatise Online 20: 1–79.

West, R.R. 2011b. Part E, Revised, Volume 4, Chapter 2C: Classification of the fossil and living hypercalcified chaetetid-type Porifera (Demospongiae). Treatise Online 22: 1–24.

Zhang, Y.L., Gong, E.P., Wilson, M.A., Guan, C.Q., Sun, B.L. and Chang, H.L. 2009. Paleoecology of a Pennsylvanian encrusting colonial rugose coral in South Guizhou, China. Palaeogeography, Palaeoclimatology, Palaeoecology 280: 507-516.

Zhang, Y.L., Gong, E.P., Wilson, M.A., Guan, C.Q.. and Sun, B.L. 2010. A large coral reef in the Pennsylvanian of Ziyun County, Guizhou (South China): The substrate and initial colonization environment of reef-building corals. Journal of Asian Earth Sciences 37: 335-349.

Zhang, Y., Gong, E., Wilson, M.A., Guan, C., Chen, X., Huang, W., Wang, D. and Miao, Z. 2017. Palaeoecology of Late Carboniferous encrusting chaetetids in North China. Palaeobiodiversity and Palaeoenvironments https://doi.org/10.1007/s12549-017-0300-5

Wooster’s Fossil of the Week: Predatory trace from the Upper Cretaceous of southwestern France

September 15th, 2017

One hole in a shell is unremarkable. Several in a repeating pattern is a story. Above is a right valve (exterior) of the oyster Pycnodonte vesicularis from the Campanian (Upper Cretaceous) of southwestern France. It was collected during our fantastic summer excursion into the Type Campanian at the Archiac location, which had beautiful exposures of the Aubeterre Formation. Note the jagged hole near the center, the subject of this post.Here is the other side of the right valve (the interior). We have multiple such examples in our collection, all in right valves and all near or on what would have been the oyster’s adductor (closing) muscle attachment. (Those of you with sharp eyes may also find some sweet Rogerella borings made by  barnacles, along with several encrusting bryozoan colonies.)A closer view of the hole showing spalled shell layers. (Also more bryozoans!)
Another close view of the above hole on the other side of the valve. It appears that these holes have been produced by some hard object punching through, spalling away the edges. This is what some predators do to shelled organisms to break them apart. Pether (1995) named the “ballistic trace” resulting from stomatopod shrimp predation as Belichnus. Cadée and de Wolf (2013) extended the range of trace makers to include seagulls. In both cases the predators essentially “spear” the shell, with the ensuing hole looking rather squarish and jagged. This is one of the “fracture-shaped bioerosion traces” in the architectural analysis of Buatois et al. (2017).

In our Cretaceous examples, the culprit was most likely some type of stomatopod (a large, diverse and long-lived group) smacking its way into the oysters through the thin right valve. Striking the muscle attachment would be the quickest way of forcing the shell open to reveal all the oysters goodness. The previously oldest example of Belichnus in the fossil record is Oligocene (David, 1997), so this occurrence extends the range back to the Late Cretaceous. That’s not a big deal because the ichnotaxon (trace fossil formal name) is relatively young and those who would look for it are very few. Its stratigraphic range is still maturing.

Update: Katherine Marenco sent this great video of mantis shrimp in action, including a “smasher”.

References:

Buatois, L., Wisshak, M., Wilson, M.A. and Mángano, G. 2017. Categories of architectural designs in trace fossils: A measure of ichnodisparity. Earth-Science Reviews 164: 102-181.

Cadée, G. C. and de Wolf, P. 2013. Belichnus traces produced on shells of the bivalve Lutraria lutraria by gulls. Ichnos 20: 15-18.

David, A. 1997. Predation by muricid gastropods on Late-Oligocene (Egerian) molluscs collected from Wind Brickyard, Eger, Hungary. Malak Táj 16: 5–12

Pether, J. 1995. Belichnus new ichnogenus, a ballistic trace on mollusc shells from the Holocene of the Benguela region, South Africa. Journal of Paleontology 69: 171-181.

 

Wildfires in Montana

September 11th, 2017

Windy, warm, and dry is a good recipe for wildfires, and that has been the norm for Montana this year.  For example, from June 1 through September 4, Missoula received 2.07 inches of precipitation, less than half its average rainfall for that period.  Most of those two inches fell by June 13, early in the fire season. The average daily temperature since June 1 has been 68.9°F, or 3.3°F higher than normal.

Cumulative precipitation in 2017 since June 1 for Missoula, MT (red) compared to average (blue).

The total acreage burned according to Inciweb is a little over 1 million acres.  Wildfires are common in western states, but this has been a particularly bad year.  The area burned is about three times the size of Wayne County, OH.

Size comparison between Wayne County, Ohio, Rhode Island land area, and the 2017 burned area in Montana as of 11 Sep 2017.

The Rice Ridge fire is one of the largest fires in Montana right now, with 135,355 acres burned as of Monday morning. According to Inciweb, It is 8% contained and has 891 personnel devoted to it. This fire has also been long-lasting; it began back on July 24th from a lightning strike. Missoula is the nearest city, but the communities of Seeley Lake and Lincoln are much closer to the fire.  Officials in Lincoln, MT have been making evacuation and fire-fighting plans.

The Rice Ridge Fire as of 11 Sep 2017. Darker red indicates more intense heat. Yellow areas are under evacuation warnings, and the dashed yellow line is the “no drones” perimeter. (Adapted from https://inciweb.nwcg.gov/incident/5414/.)

Glacier National Park, already with over 16,000 acres burned from the Sprague Fire and the Adair Ridge Fire, added one more active fire to the list on Saturday when a human-caused fire over the border in Canada spread into the northwest corner of the park.  The Elder Creek fire has burned 211 acres in the USA so far, but it is considered low priority given its remote location. The Park recently lost the historic Sperry Park Chalet, built in 1914, to the flames.  With warm, dry, windy conditions expected to continue in the short-term, the fire damage for Montana and other western states is likely to increase.

Weather data from the National Centers for Environmental Information (https://www.ncdc.noaa.gov)

The annual Wooster Paleontology field trip to the Upper Ordovician (Fall 2017 version)

September 10th, 2017

It’s not that I haven’t loved all my Invertebrate Paleontology classes, but the students this year are special because there are only ten of them. Lately I’ve had up to thirty students per class which is great for many reasons, but running field trips is not one of them. With ten students we can go places buses can’t, and I can pay closer attention to what each student is experiencing. Today’s field trip to an exposure of the Upper Ordovician lower Whitewater Formation near Richmond, Indiana, was delightful. (C/W-148; N 39.78722°, W 84.90166° — which has a nice Google Maps street view.)

The stratigraphy here is very simple and well delineated by generations of geologists. All the students need to do is collect fossils. They don’t know much about them yet because the course has just started, so their collections will be the basis of ongoing preservation and identification projects. Here we see Meredith Bruch and Victoria Race (below) finding goodies, while Fox Meyer climbs up the talus pursuing fabulous fossils.

Our geological technician Nick Wiesenberg went along as a driver and an ace fossil collector with an excellent eye, which I learned about when he helped Team Minnesota last year.

Ann Wilkinson enjoys the wonders of roadside geology in the Midwest.

Here’s a nice representative slab Fox collected of the fossils at this location. Brachiopods, bryozoans, and bivalves dominate the fauna.

Every student had a tray awaiting him or her on return to Wooster.

And the students did their work. Now each needs two trays. They will begin this week washing, labeling and sorting their specimens. Then they start identifying, using among other sources the excellent Digital Atlas of Ordovician Life and Cincinnatian Strata websites.

As a bonus, below is part of the 2007 Invertebrate Paleontology class on the same outcrop. Some alumni may recognize themselves, even though they are in classical paleontological poses.

Wooster’s Fossil of the Week: A rudist clam from the Upper Cretaceous of southwestern France

September 8th, 2017

When we picked up this beautiful fossil in southwestern France this summer, Paul Taylor immediately predicted it would become a Wooster Fossil of the Week. Macy Conrad (’18), Paul and I were on our wonderful expedition in the Type Campanian (Upper Cretaceous) of France. Paul took us to a most unpromising plowed field, claiming there were fossils here from the Maurens Formation. Sure enough we found a pile of large fossils that farmers had picked from their fields. They included probably the most distinctive invertebrate organism of the Late Cretaceous: the rudist clam. Hard to believe these conical objects were clams, but such is evolution. (They have the disconcerting shape and size of other objects found in some French fields: artillery shells!)

The cone itself is the right valve of these sedentary bivalves. The capping valve is the left, as seen here from the top. (Right and left make little sense unless you think of their more traditional bivalved ancestors.) Note that this valve has a reticulate, almost lacy pattern to the shell. Rudists were filter-feeders like most bivalves, but they may have also supplemented their nutrition with photosynthetic symbionts in their mantle tissue. The holes in the top valve may have allowed sunlight to hit the upper mantle.

This stratigraphic chart, courtesy of Platel et al. (1999) via Paul Taylor, shows the Maurens Formation at the top of the Campanian in southwestern France. Our primary Campanian work in SW France is with the three units below (the Biron, Barbezieux and Aubeterre formations).

A typical heterodont clam is in the upper left of this diagram; the rest are elaborate rudist clams. In the lower right is a drawing of the type of rudist photographed above. Diagram from Schumann & Steuber (1997).

Rudists flourished in Cretaceous seas right up until the mass extinction at the end of the period. They are often characterized as reef builders, but most were probably living on soft sediment substrates, like our friend here.

References:

Gili, E., Masse, J.P. and Skelton, P.W. 1995. Rudists as gregarious sediment-dwellers, not reef-builders, on Cretaceous carbonate platforms. Palaeogeography, Palaeoclimatology, Palaeoecology 118: 245-267.

Platel, J.-P. 1996. Stratigraphie, seédimentologie et évolution géodynamique de la plate-forme carbonatée du Crétacé supérieur du nord du basin d’Aquitaine. Géologie de la France 4: 33-58.

Platel, J.-P., Faugeras, P., Mauroux, B., Spencer, C., Charnet, F., Célerier, G., Harielle, B. and Jacquement, P. 1999. Notice explicative, Carte géologie France (1/50 000), feuille Thenon, Orléans, BRGM, 128 p.

Schumann, D. and Steuber, T. 1997. Rudisten. Erfolgreiche Siedler und Riffbauer der Kreidezeit. Städte unter Wasser-2 Milliarden Jahre.-Kleine Senckenberg-Reihe 24: 117-122.

Steuber, T., Mitchell, S.F., Buhl, D., Gunter, G. and Kasper, H. U. 2002. Catastrophic extinction of Caribbean rudist bivalves at the Cretaceous-Tertiary boundary. Geology 30: 999-1002.

Unknown fossils for the Invertebrate Paleontology class at Wooster

September 1st, 2017

I start my Invertebrate Paleontology classes with an unknown fossil given to each student. I pick something I have enough examples of so that everyone gets the same species. As their first assignment, the students are asked to identify their fossils as specifically as possible using whatever method works, short of asking me or my teaching assistant. Once they’ve identified their specimens, they are then asked to provide an age and likely location of collection. The beautiful fossils above were the unknowns for this semester’s class. Do you know what they are?

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These are specimens of the trepostome bryozoan Prasopora falesi (James, 1884) from the Decorah Formation (Katian, Upper Ordovician) of Decorah, Iowa. They were collected by Rachel Wetzel (’17) as part of our Team Minnesota expedition in 2016. Four of my current students figured this out to the species level! Most knew we were in bryozoan territory.

Jesse Davenport (’11) Returns to GeoClub

August 31st, 2017

Wooster, OH – GeoClub met for the first time in the 2017-2018 academic year, allowing us to catch up with old friends and meet new ones. It was our good fortune to host a special guest, Jesse Davenport, a 2011 Wooster Geology graduate. He joined us for GeoClub lunch in Lowry, reminiscing about his time at Wooster and sharing his story of life after graduation. As a special favor, he agreed to write a post about his experiences for the Wooster Geologists. Thanks, Jesse! If you’re a Wooster Geology graduate and would like to share your story, please contact Dr. Meagen Pollock.

Jesse Davenport (’11) visited the first meeting of GeoClub and shared his experiences of life after graduation.

 

Since Wooster, lots of thing have happened, traveling, seeing new places, meeting new, interesting people, discovering new cultures and many other things. After I graduated from Wooster, in 2011, I went on to the University of Notre Dame where I pursued a Masters degree in lunar geochemistry for two years. After this, I worked various jobs, but at the same time was searching for what would come next, whether it was a real job in some sort of geological field, a PhD program or even something else. After a few options fell through or where not that appealing I decided to apply for a PhD position that I had seen on the internet in Nancy, France (located between Paris and Strasbourg). I really didn’t know what to expect and to be honest, I thought that my skype interview with my potential advisors was the worst interview that I had ever done. But, despite this, they accepted me and with nothing else in mind that was interesting, I decided to accept this position. Now, I am not one to complain about things, but you do not know what paperwork is like until you have lived as a foreigner in France (or maybe just in any foreign country in general). It was nightmare, plus add on top of that not being able to speak French, all the culture shock and you get a scenario that would send most be people running. I stuck it out though and here I am four years later, I am almost finished with my thesis.

My PhD topic focuses around the  dynamics of weathering and erosion in the Himalayas. In the early 1990s a huge debate began, at the advent of the Ocean Drilling Program from which we now had access to oceanic records that spanned millions of years, about what are the interactions between climate, tectonics, erosion and weathering and whether that has spurred the changes we see on the Earth throughout the past 5 million years. One of the biggest questions in the Himalaya is that we would like to know how uplift and erosion has affected the global concentrations of carbon dioxide throughout the past 50 millions years. Silicate weathering (along with organic carbon burial) is one of the mechanism that mother nature uses to regulate the the amount of carbon dioxide in our atmosphere. Of course, we have had eras where these levels have been higher or lower, depending on the situation at that moment, but in general silicate weathering is the process that controls these levels. So, my PhD focuses on the isotope geochemistry of sediments, rivers and other material in the Himalaya to try to understand how the Himalaya, at present, function with respect to the dynamics between erosion, weathering and climate.

Wooster Geology Department 2017 Annual Report

August 28th, 2017

The Thirty-First Annual Report of the Geology Department is now available online with this link. Our Administrative Coordinator Patrice Reeder has once again done a magnificent job putting this document together, with amazing attention to detail and an artistic eye for format and style. Read and enjoy!

Wooster’s Fossils of the Week: Oysters from the Upper Cretaceous (Campanian) of southwestern France

August 22nd, 2017

Wooster’s Fossil of the Week returns from its summer hiatus. It is appropriate, then, to feature as our first fossil of the new season an oyster species prominent in our summer research. This is Pycnodonte vesicularis (Lamarck, 1806), a very common fossil in the Cretaceous around the world. These particular specimens are from the Aubeterre Formation (Upper Campanian, Upper Cretaceous) exposed in the town of Archiac in southwestern France. They were collected by Macy Conrad (’18), Paul Taylor (Natural History Museum, London) and me during our June 2017 expedition. Above is the interior of a deeply concave left valve. The large spot near the middle is the single adductor muscle scar (thus the oyster, like all oysters, is monomyarian). It was a free-living oyster in soft, shallow platform marine sediments. This species has been used for all sorts of studies, from investigating paleoecology and evolution to paleoseasonality (see references below for a start).

This is the interior of the right valve, showing the corresponding muscle scar. The valves are very different in size and shape, so this oyster is termed inequivalved.The exterior of the right valve, with characteristic faint radiating ridges. The tag, by the way, indicates the locality. Every one of our hundreds of oysters is tagged in this way.Macy Conrad (’18) is seen here at the Archiac outcrop collecting specimens of Pycnodonte vesicularis.

A typical bed of P. vesicularis in the Upper Campanian of SW France. This one is exposed along the sea cliffs at Pointe de Suzac.

References:

Brezina, S.S., Romero, M.V., Casadío, S. and Bremec, C. 2014. Boring polychaetes associated with Pycnodonte (Phygraea) vesicularis (Lamarck) from the Upper Cretaceous of Patagonia. A case of commensalism? Ameghiniana 51129-140.

De Winter, N.J., Vellekoop, J., Vorsselmans, R., Golreihan, A., Petersen, S.V., Meyer, K.W., Speijer, R.P. and Claeys, P. 2017. Cretaceous honeycomb oysters (Pycnodonte vesicularis) as palaeoseasonality records: A multi-proxy study. EGU General Assembly Conference Abstracts 19: 4359.

Lamarck, J.B. 1806. Suite des mémoires sur les fossiles des environs de Paris. Annales du Muséum National d’Histoire Naturelle 7: 130-139.

Platel, J.-P. 1996. Stratigraphie, seédimentologie et évolution géodynamique de la plate-forme carbonatée du Crétacé supérieur du nord du basin d’Aquitaine. Géologie de la France 4: 33-58.

Videt, B. 2003. Dynamique des paléoenvironnements à huîtres du Crétacé supérieur nord-aquitain (SO France) et du Mio-Pliocène andalou (SE Espagne): biodiversité, analyse séquentielle, biogéochimie (Doctoral dissertation, Université Rennes 1).

Wooster Geology Professor Frederick W. Cropp III (1932-2017)

August 11th, 2017

Professor Fred Cropp taught geology at Wooster from 1964 to 1997. He was an extraordinary teacher and, in his own words, “a cheerleader for geology”. Many, many Wooster students became geologists in response to his enthusiasm, energy and spirit. I was one of them. His obituary and memorial page is here.

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