And sometimes it rains.

Today I took Peter, Lauren and Evie on another afternoon local field trip, this time to Wooster Memorial Park (Spangler). We wanted to repeat the enjoyable exploration we had last week in Lodi Community Park. This time, though, we got thoroughly drenched by a small thunderstorm cell that just seemed to hover over us. The students managed to get these images.

It started out well! Evie and Lauren found salamanders in the creek bed.

But then the rain got serious!

It was a steady downpour, forcing us to exit once we were thoroughly soaked.

The trails became streams on our hike back to the car. Still, it was a fun adventure, if a bit short!

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Klawock to Ketchikan

Guest bloggers: Amanda Flory and Mihalis Protopapadakis

Carnivorous sundews found in Balls Lake muskegs.

On our last full day at Prince of Wales Island, we explored the trail around Balls Lake, in Tongass National Forest. The AYS team helped us core trees of several different species. We then returned to the AYS headquarters in Klawock and taught them how to mount tree cores and analyze them under the microscope. We also celebrated Nick’s birthday!

The following morning we took the ferry back to Ketchikan and spent the day climbing Dude Mountain. There, we collected more cedar samples in a muskeg and a bear trail along the edge of a cliff. We spent the final day of our trip exploring the city of Ketchikan and the nearby beaches.

Bob and Dr. Wiles searching for cedars in the rainforest.

Salmon-spawing stream flowing out of Balls Lake.

Gary supervising tree-core collection at a Forest Service site.

The Wooster team and AYS group deep in the woods of Balls Lake.

Gary’s cedar cookie showcasing abnormal ring characteristics.

Freshly picked blueberries.

The team hiking along the Balls Lake trail.

The team skillfully balancing on a slippery log.

Teaching the AYS group how to process and examine tree cores back at headquarters.

The team sharing excitement over dendrochronology.

Celebrating Nick’s birthday with a delicious cake that David baked.

Happy Birthday Nick!

A bald eagle spotted on the drive to Dude Mountain.

Couple of dudes on Dude Mountain.

The view from the bear trail along the cliff.

Amanda and Proto coring a yellow cedar.

The famous Creek Street boardwalk in southern Ketchikan.

The view from the team’s airbnb.

On the final day, the team visited tidal pools along the coast.

A starfish saved from low tide.

This trip was a wonderful experience. Thank you to all the great people we met along the way! Also a big thank you to Dr. Wiles and Nick for their guidance and these great memories. A big thank you to Bob Girt and the Alaska Youth Stewards Group in Klawock who hosted our trip on Prince of Wales Island. This work was supported by Grant NSF P2C2-2002454 and the Department of Earth Sciences at Wooster.

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54 cm Core from Brown’s Lake Bog Reveals …

Guest Bloggers: Evie Sanford and Peter Rothstein

Summer diatom research continues at The College of Wooster. Building on last summer’s work by Garret Robertson, Minnie Pozefsky and Dr. Mark Wilson, as well as that of other previous IS students Justine Paul Berina and Richard Torres, we have been analyzing the diatom communities at Brown’s Lake. Brown’s Lake is well known among Wooster geology students as the site for many IS projects, research expeditions and class field trips. Located within a Nature Conservancy protected area, the lake is a remnant from glacial ice left behind from retreating glaciers ~15,000 years ago.

A LIDAR map of Brown’s Lake Bog Nature Preserve.

After a hot, muddy expedition to the lake in mid-June, we ended up with a sediment core from the edge of the lake. Thanks to Dr. Wiles and Nick Wiesenberg for helping us out with obtaining the core!

The 54 cm core retrieved from Brown’s Lake.

The core we ended up with is 54 cm long, and composed of mostly peat. The core has not been dated, but likely extends to around the mid-19th century based on a more silt-heavy composition in the lower sections of the core. Last year’s team was able to match this silt deposition to effects of European-American settlement in the area. Our objective was to further investigate the impacts that this silt deposition and anthropogenic impacts had on diatom communities in Brown’s Lake by surveying their abundances over different depths.

Evie took the lead on making smear slides, following the procedure from Richard Torres’ IS. Taking a sediment sample every 5 centimeters and isolating the silicates. This left behind the diatom skeletons and sponge spicules we wanted to study.

Scientific marbles!! (boiling our hydrogen peroxide and homogenized water-soil sample to kill the organics).

Spinning the samples in the centrifuge to isolate diatoms within the leftover solution.

Our slides prepared for inspection.

After isolating all of the diatoms, we got started on counting them. Peter looked at each smear slide by looking over it 3 times and recording the diatom genera that were intact enough to make an identification. In total 461 individual diatoms and 17 genera were found within the 54 cm core. We found that diatom abundance and diversity peak at a depth of 5 cm to 10 cm and decrease significantly with core depth.

Total diatom count by depth.

Common diatom genera found in BLB smear slides.

In addition to measuring abundance and diversity of diatoms, we looked at the Biological Condition Gradient of the diatom genera observed. Biological Condition Gradient is a conceptual measurement of ecosystem function/disruption. It ranges from 1-6, with 1 being a wholly natural community structure and 6 being extreme ecosystem disruption. During the section of the core with high silt deposition, Melosira and Navicula are the most common genera. Melosira is largely present in environments with BCG 4 and Navicula are generalists, spread from BCG 1 to 5. However, in the peaty layers near the top of the core, BCG ratings for diatom genera that are usually only present in ecosystems with BCG of 3 or lower. This would indicate that the Brown’s Lake ecosystem has rebounded from the previous environmental disruption.

Diatoms weren’t the only siliceous microfossils present in the core. We also found the occasional sponge spicule:

This core is important to ongoing research at The College of Wooster because it is a subrecent core containing the most recent sediment including diatom skeletons (frustules) and sponge spicules.

Acknowledgements

We thank Nick Wiesenberg for his help both in the field and retrieving the core and instruction in the laboratories. Additionally, we thank Dr. Greg Wiles for his experience and leadership on this project. Previous College of Wooster students Justine Paul Berina, Richard Torres, and Garrett Robertson, as well as Williams College student Minnie Pozefsky, developed and refined many of the techniques used in this work. This investigation was funded by the National Science Foundation grant #2039939.

 

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A local geological field trip on a midsummer’s day: Return to the Lower Carboniferous of Lodi, Ohio

Wooster, Ohio– This afternoon three industrious summer research students and I took advantage of the brilliant weather to drive 30 minutes north of town to Lodi Community Park in Medina County, Ohio. We wanted to take a break from lab work and writing to explore for interesting rocks and fossils. I also wanted to revisit the outcrops because of some new interest in the fossils by colleagues. I was last at this site eleven years ago with a Sedimentology & Stratigraphy class.

Lodi Community Park has a narrow valley through which flows the East Fork of the Black River. (The depth of the valley indicates it was originally cut by a much larger river in the waning days of the Pleistocene ice sheets.) Along the cutbanks of the river are exposures of the Meadville Shale, a member of the Cuyahoga Formation. It is Lower Carboniferous (Mississippian) of the Kinderhookian Stage. The stream bed contains rocks derived from the cliffs on each side, along with the occasional glacial erratic.

Three of our ace summer research students went with me to Lodi for this short trip. From the left, Peter Rothstein, Lauren Segura, and Evie Sanford. Peter and Evie are currently working on diatoms and sponges in Brown’s Lake, and Lauren is in the Wooster Tree-Ring Lab this summer. Behind them is an outcrop of the Meadville Shale, which here consists of poorly-resistant gray shale at the base and layers of micaceous quartzose siltstones that are more resistant. The wooden pole in the background, by the way, is a Jacob’s Staff used to measure stratigraphic columns. Each interval is 10 cm. I painted this staff when I was a new professor because I couldn’t find any metric versions in the United States!

Evie is here scanning the stream bed for fossils and interesting rocks. (Thank you again for driving, Evie!)

Lauren was almost always in the water when I looked.

Peter  was very intent in his rock-scanning. All three students made interesting finds.

This is a typical siltstone from the Meadville Shale at Lodi. It is full of branching bryozoan colonies (zoaria).

The underside of this siltstone slab shows numerous trace fossils. Their preservation is termed convex hyporelief.

Siderite beds and concretions are common in these Lodi exposures. In this loose boulder we can see the red-brown siderite with trace fossils at the base overlain by thin beds of fine calcareous fossil debris.

This is an internal mold of a productid brachiopod. It has just a little bit of original calcite remaining from the shell. The arrow indicates hollow spines, which are characteristic of productids. It is rare to have them preserved since they are very fragile. The scale is in millimeters.

There were a few small solitary rugose coral skeletons with their original calcite. On the right is another productid brachiopod, this time as an external mold with some original calcite remaining. Some spines are visible.

This could have been the specimen of the day but for the vagaries of preservation. This is a siderite concretion with a nearly complete crinoid. Its articulated stem (column) is easy to see on the left above the scale bar. On the right are the remnants of what would have been an entire crown with multiple feeding arms. Unfortunately this crown is eroded into a vague cross-section. It is preserved in the same manner as this contemporary specimen described in this blog.

This post gives me a chance to mention how this Lodi fossil locality began my career as a paleontologist. The fossil above, shown as a reversed stereo-pair, is an external mold of a trilobite cephalon. It was found in 1977 by College of Wooster student Mary Beidler. I was also a Wooster student at the time, so Mary gave it to me to identify. I was thrilled because Carboniferous trilobites are uncommon. I could, though, only classify it to the genus Brachymetopus. Turns out it was a new species, which I named in a short 1979 paper as Brachymetopus nodosus. This was my first publication. Thank you again, Mary!

There were some big spiders under the rocks! (Photo by Evie.)

Another change since my last visit — a fancy new bridge over the stream! Back in the day it was a low concrete weir that flooded quickly, sometimes trapping people in the park. This nice bridge was opened just a couple of months ago.

Thanks again to Peter, Lauren and Evie for a great afternoon of field geology!

Reference:

Wilson, M.A. 1979. A new species of the trilobite Brachymetopus from the Cuyahoga Formation (Lower Mississippian) of northeastern Ohio. Journal of Paleontology 53: 221-223.

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Ketchikan to Klawock

Guest Bloggers: Mihalis Protopapadakis and Amanda Flory

This year the College of Wooster Tree Ring Lab flew to Ketchikan for our 2024 Alaska trip. July 6th and 7th were spent in Ketchikan, where we collected samples from Deer Mountain after a rigorous hike. On July 8th we took a ferry to Prince of Wales Island, where we collaborated with Alaska Youth Stewards in the city of Klawock to create a new tree-ring record of the region. While in Klawock, we had the opportunity to bond with the AYS team and explore the local Tlingit culture.

The city of Ketchikan on a rare sunny day.

The Wooster team in front of a Tlingit totem pole.

The view from halfway up Deer Mountain.

Dr. Wiles riding the saddleback of two cedars.

The Wooster team hard at work.

Sun-rays peeking through remnants of possible staurolite crystals in the phyllite bedrock.

The Deer Mountain tree-ring data up to 1998. The chronology highlights the volcanic eruptions of the 1690s and 1809, extending the tail-end of the Little Ice Age. The team collected samples to update the record with the last 25 years.

Kite surfer catching the waves of the ferry to Prince of Wales island.

Meeting the AYS team and other collaborators in Klawock.

The team after a hard day’s work, in front of a magnificent yellow cedar.

The Wooster team coring a dead cedar deep in the mountains.

The AYS experts coring a cedar.

Bob, the instructor of the AYS group, posing with style.

The temperate rainforest around Klawock.

A beautiful moth posing on cedar.

Old logging road on the way to our second site of the day.

Monument of chainsaws by the team’s airbnb.

We spent our third day in Klawock at the Craig Tribal Association’s Culture Camp.

Nick and Proto carving traditional halibut hooks.

After the Culture Camp, we visited Sealaska’s totem tree yard to collect more samples.

Marked totem log, soon to be sent off to Alaskan artist DB.

Proto coring an enormous cedar log (could not reach the middle).A big thank you to Bob Girt and the Alaska Youth Stewards Group in Klawock who hosted our trip on Prince of Wales Island. This work was supported by grant NSF P2C2-2002454 and the Department of Earth Sciences at Wooster.

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Two Environmental Geoscience majors featured in Wooster Magazine

We are proud of all our graduating seniors. When their Senior Independent Study projects are described outside the department, we highlight their excellent work for a larger audience. Corey Knauf (shown above) and Athena Tharenos (shown below) were both featured in the Summer 2024 edition of Wooster Magazine. We hope you can read their IS stories at the link. These beautiful images were taken by our ace college photographer Matt Dilyard.

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Buggin’ Out at Apple Creek

 

Guest Bloggers: Evie Sanford and Peter Rothstein – On June 11, the 2024 Scovel Summer Research Team visited Apple Creek with Trout Unlimited to analyze the water quality through a macroinvertebrate survey. This study was performed because macroinvertebrates are often used as biological indicators of stream quality due to their response to pollution. Special thanks to Carrie Elvey from OSU CFAES for teaching us about the area, the method, and what it all means for conservation efforts.

Our 2024 collection team!

The team used the kick seine method and dip nets to collect macroinvertebrates from the stream.

In addition to nets, we flipped over rocks to find organisms like leeches, water pennies, and macroinvertebrate larvae.

Carrie taught us about the types of organisms we found.

Final tray for site one

Rainbow Darter (Etheostoma caeruleum)

Mayfly Nymph

Water Penny (Psephenidae sp.)

Site 1 Pollution Tolerance Index by year for the past 12 years. The lowest rating was 27, meaning PTI was excellent for every year measured.

 

Site 2 Pollution Tolerance Index by year for the past 12 years. The lowest value recorded, November 2013, had a value of 21, indicating good water quality. Other than that, the stream recorded excellent or better water quality throughout the recorded measurements.

Original data sheets were collected for sites 1 (left) and 2 (right).

The stream continues to receive a ranking of excellent – the highest possible rating. This excellent stream health rating for Apple Creek indicates a bright future for the stream.

In addition to the macroinvertebrate survey and our calculated pollution tolerance index, we compiled data from data loggers installed in the stream.

 

Apple Creek graph showing temperature in blue (ºC) and water levels in black (kPa) measured from a data logger in the stream channel itself. As expected, temperatures fluctuate by season, while water levels change over a shorter time frame. Note that storm events (peaks in water levels) are associated with warmer temperatures in the warm summer months and colder temperatures in the winter/early spring. These data were taken every hour.

 

Apple Creek 2 showing the temperature in blue (ºC) and water levels (kPa) when a new logger was implemented into a well casing that was installed into the stream bank approximately 10 feet from the channel and about 5 feet deep. In the coming years keeping track of the physical aspects of water flow and temperature should add to the story of environmental and water quality of Apple Creek monitoring efforts by Trout Unlimited, CFAES, and The College of Wooster.  

 

 

 

 

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James Parkinson, Paleontologist

Ann Arbor, Michigan — This morning I gave a talk at the North American Paleontological Convention (NAPC) about the extensive contributions that the English physician James Parkinson (1755-1824) made to the rapidly growing field of paleontology in the early 19th century. This was initially a surprise to me. I had earlier this year looked up details on the life of Parkinson because he is the namesake for Parkinson’s Disease, but was astonished to learn that he had published extensively on fossils. I joined with co-authors Bill Ausich (The Ohio State University) and Caroline Buttler (National Museum Wales) to explore Parkinson’s life and work and bring him to the attention of a new generation of paleontologists. We saw that Parkinson has been nearly forgotten in modern paleontology despite numerous prescient ideas. I’ve taken the PowerPoint slides of the presentation, removed the animations, and made it into the series of images here. I think they have enough text to convey an outline of Parkinson’s paleontology.

Thank you to my Israeli friend and colleague Yael Leshno Afriat for taking this image of me speaking at the NAPC session. This is the first talk I’ve ever given anywhere without a tie and jacket!

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Twisty little encrusting tubeworms: A new paper describes two new Jurassic spirorbin species, pushing back the origin of the group and giving us a nice paleoecological evolution narrative.

Several of my colleagues and I have been studying the fossil records of tubeworms for almost three decades now. We find them especially interesting because they are often beautifully preserved on hard substrates like shells, rocks and hardgrounds. They represent a relatively simply paleoecological niche: small sessile benthic filter-feeders. Tubeworms are also systematically diverse and polyphyletic (no common tubeworm ancestor). They show much evolutionary convergence over time between separate groups. One of the most dramatic comparisons (if there is drama in such esoteric topics) is between the extinct microconchids and the extant spirorbin serpulids. Their little shells can be nearly identical, separable primarily bu different skeletal microstructures. Microconchids and spirorbins are in the same ecological niche, but when did the former give way to the latter? We now have new evidence that narrows the time gap between the two clades.

Two years ago I had a look through a set of crinoid columns collected in the Callovian (Middle Jurassic) Matmor Formation of southern Israel. The fantastic fossils in the Matmor have been the basis of many papers (and blog posts) from my research group over the past two decades. (The top image of this post shows some of these fossils in the field. Note the abundant crinoid columns.) I was revisiting these crinoid columns for some crinoid-related idea I’ve now forgotten. Instead, I noticed tiny little spiral tubeworms encrusting some of the crinoids. This was immediately an issue — they were either the youngest microconchids (which are Bathonian, a stage below) or the oldest spirorbins (up until now in the Cretaceous, a system above). They fell into the stratigraphic gap between these groups.

I sent the specimens immediately to my friend and colleague Olev Vinn in Estonia. He determined through analysis of the microstructure that these Callovian tubes were of the earliest spirorbins, and that they represented two new species. We invited two other experts into the project who had their own mysterious Middle Jurassic tubeworms. Our paper has now appeared in the journal PalZ. Here is the abstract —

Two new spirorbin species, Neomicrorbis israelicus sp. nov. and Spirorbis? hagadolensis sp. nov., are here described from the Callovian of Israel, together with two new variations of Neomicrorbis israelicus from the late Bathonian of northern France and Callovian of Madagascar. These are the geologically earliest true Spirorbinae. Our new data, and a literature review of microconchids and early spirorbins, suggest that the ecological switchover from spirorbiform microconchids to spirorbin polychaetes took place in the late Bathonian, and that the spread of spirorbins across the Jurassic and Early Cretaceous seas was rapid. The ecospace of spirally coiled spirorbiform microconchids could thus have been competitively taken over by true spirorbins. The true spirorbin polychaetes may have been ecologically more successful than their Paleozoic analogues – the microconchids. The general rarity of spirorbin-bearing localities in Europe from the Bathonian to Albian supports the hypothesis that the Spirorbinae likely originated in the equatorial Tethys and only occasionally spread to the northern hemisphere seas until the end of the Early Cretaceous. Spirorbins finally became common, diverse and widespread in the northern seas by the Late Cretaceous, and even more so in the Cenozoic.

Spirorbins from the Callovian of Hamakhtesh Hagadol, Israel. a Longitudinal section of the tube showing growth lamellae characteristic of the serpulids. b Section through the tube showing open tube origin and lack of protoconch. c Neomicrorbis israelicus sp. nov. encrusting a crinoid stem. d–e Neomicrorbis israelicus sp. nov. (holotype) showing four longitudinal keels. f. Neomicrorbis israelicus sp. nov. (paratype). Scale bars: a, b, e, f 300 um; c 5 mm; d 400 um. (From Figure 1 of Vinn et al., 2024.)

a–d Spirorbis? hagadolensis sp. nov. from the Callovian of Hamakhtesh Hagadol, Israel. Note lack of the longitudinal keels and rounded tube cross-section. Scale bars: a 400 um; b 200 um; c, d 300 um. (From Figure 4 of Vinn et al., 2024.)

I tell my students to always look for anomalies in scientific observations and data. There are stories to be told when you find something out of place. This is also a case of specimens in a collection being useful for projects unknown at the time they were gathered. This is one reason why have museums to preserve items for unknown future discoveries. The spirobin tubeworms here are certainly not charismatic fossils, but they nonetheless fill in an important evolutionary gap.

Reference:

Vinn, O. Wilson, M.A., Jäger, M. and Kočí, T. 2024. The earliest true Spirorbinae from the late Bathonian and Callovian (Middle Jurassic) of France, Israel and Madagascar. PalZ (in press) https://doi.org/10.1007/s12542-023-00681-7

 

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Examining Late Cretaceous (Maastrichtian) North American dinosaur teeth and their palaeoecological implications in the Hell Creek Formation of Carter County, Montana – The Independent Study project of Hudson Davis (’24)

Editor’s Note: Independent Study (IS) at The College of Wooster is a three-course series required of every student before graduation. Earth Sciences students typically begin in the second semester of their junior years with project identification, literature review, and a thesis essentially setting out the hypotheses and parameters of the work. Most students do fieldwork or lab work to collect data, and then spend their senior years finishing extensive Senior I.S. theses. The following is Hudson’s thesis abstract —

The Hell Creek Formation is an iconic Late Cretaceous formation that is found throughout the states of Montana, Wyoming, and the Dakotas. Even though it has been studied for over 100 years, questions about the paleoecosytem it represents still need further research. I here examine dinosaur teeth from the Hell Creek of Carter County, Montana, a section that is understudied compared to other exposures of the formation. While many studies focus on the dinosaur fauna of this ecosystem, most of these studies focus on skeletal material. Dinosaur teeth are abundant within microvertebrate sites in the Hell Creek, and these teeth can tell and confirm similar information to that of the skeletal remains, while also providing information that preservation bias might otherwise obscure. By conducting a tooth census comprised of 1,505 dinosaur teeth and comparing that to similar skeletal censuses, I hypothesize that while certain fauna like Triceratops will, as reflected in the skeletal record, be the most abundant tooth taxa, other species not as common from skeletal remains, such as dromaeosaurs, will be more common from teeth surveys, as their hollow bones are subject to preservation bias. I also predict that different lithologies of microsites will contain different teeth assemblages due to niche partitioning within the environment.

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