Climate Change Class at Secrest Arboretum

Adrian (Philosophy) and Kelly (Geology) core a European Larch for an ecological response study using tree-rings

Adrian (Philosophy) and Kelly (Geology) core a European Larch for an ecological response study using tree-rings. The class will compare how various trees are responding to climate variability over the last 100 years or so. The site is the Secrest Arboretum of Ohio State University's OARDC. We thank Ken Cochran, Director of the facility for permission to do this study.

Chesea and Adonic core a Norway Spruce

Chesea (Archaeology) and Adonis (Political Science) core a Norway Spruce

Houston and Roz sneak up on a Pondersosa Pine and obtain a core

Houston (Religious Studies) and Roz (Archaeology) sneak up on a Pondersosa Pine and obtain a core

Travis and Adrian at the OARDC Meteorolgical Station. After the class develops tree-ring chronologies they will compare the ring-width series to the long (>100 year) record of monthly temperature and precipitation records from this site.

Travis and Adrian at the OARDC Meteorological Station. After the class develops tree-ring chronologies they will compare the ring-width series to the long (>100 year) record of monthly temperature and precipitation records from this site.

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Mineralogy-Structure Field Trip to Pennsylvania

Last weekend, Dr. Judge’s and Dr. Pollock’s Structure and Mineralogy classes took a field trip to central Pennsylvania. It rained on Saturday, but that didn’t stop us from having a great time. We saw the most amazing pencil structures in the Reedsville Shale.

The intersection of cleavage and bedding create "pencils."

The intersection of cleavage and bedding in the Reedsville Shale creates "pencils."

In the Bald Eagle Formation just a short drive down the road, we found textbook examples of slickenfibres. Slickenfibres are elongated minerals that grow along a fault plane parallel to the direction of motion.

Colin Mennett, Dr. Shelley Judge, Megan Innis, Becky Alcorn, and Andrew Retzler excited about slicken-fibers along a fault surface in the Bald Eagle Formation.

Colin Mennett, Dr. Shelley Judge, Megan Innis, Becky Alcorn, and Andrew Retzler are excited about slickenfibres along a fault surface in the Bald Eagle Formation.

Close-up view of the slicken-fibres.

Close-up view of the slicken-fibres.

Next, we went to the Bear Valley Strip Mine. The beautifully exposed folds and giant iron concretions are simply breathtaking!

Bear Valley Strip Mine. Notice the person in the yellow jacket (center of the picture) for scale.

Bear Valley Strip Mine. Notice the person in the black jacket (center of the picture) for scale.

Finally, we stopped to sample some (very orange) acid mine drainage at a nearby pump slope.

Palmer Shonk and Becky Alcorn standing beside a river full of "yellow boy," an iron hydroxide phase that is precipitating from acid mine drainage.

Palmer Shonk and Becky Alcorn standing beside a river full of "yellow boy," an iron hydroxide phase that is precipitating from acid mine drainage.

Become a fan of the College of Wooster Geology Department page on Facebook and see more photos from this trip!

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Wooster Geologist = NPR Star

Tree rings, Lake Erie, and climate change are the topics of a recent NPR interview with Wooster’s own Greg Wiles. Greg and his research group have been making headlines for their study that suggests natural climate variability plays a role in controlling changes in Lake Erie’s level. Stay tuned for more developments from Wooster’s Tree Ring Lab!

From the Guardian, May 14, 2009 issue.

From the Guardian, May 14, 2009 issue.

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End of Wooster Israeli Fieldwork — For Now

MITZPE RAMON, ISRAEL–After today’s work near Makhtesh Ramon, our fieldwork is over for this season.  This evening I pack up our collections in my luggage, have a last dinner with Yoav and his family in their desert home, and then get some sleep before a very early departure tomorrow morning.  I am looking forward to returning soon with Wooster Independent Study students to continue our work in the Mesozoic rocks of southern Israel.

A Bronze Age tumulus (rock-covered grave) at the top of a hill north of Makhtesh Ramon.

A Bronze Age tumulus (rock-covered grave) at the top of a hill north of Makhtesh Ramon.

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A Bit of Vertebrate Paleontology

MAKHTESH RAMON, ISRAEL–On my last day of fieldwork Yoav took me to some wonderfully complex exposures of Cretaceous and Tertiary rocks just north of Makhtesh Ramon. They tell a story of the origins of the Makhtesh anticlinal structure, especially the date it appeared and whether it was ever exposed as an island before its center was eroded away. Part of the debate comes down to the depth at which certain Santonian (Cretaceous) sediments were deposited. These sediments contain oysters and exquisite shark’s teeth. We collected a nice set (see below) which I will attempt to identify to see if we can use what we may know about these sharks to determine the depth of deposition.

Cretaceous shark teeth collected from just north of Makhtesh Ramon (N30.56235°, E34.64876°).

Cretaceous shark teeth collected from just north of Makhtesh Ramon (N30.56235°, E34.64876°).

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Wading in the Jurassic Sea

Another indication of how shallow the seas were in the Middle Jurassic of southern Israel.  This bedding plane in the Matmor Formation of Makhtesh Gadol has a gastropod (snail) fossil in the center of the image surrounded by angular shells of fossil mytilids (clams commonly called mussels today).  In life the mytilids had attached to the gastropod and each other by fine yet strong byssal thread produced by a special gland.  This kind of relationship is very common in tidal pools and other shallow areas where wave action is strong.

Another indication of how shallow the seas were in the Middle Jurassic of southern Israel. This bedding plane in the Matmor Formation of Makhtesh Gadol has a gastropod (snail) fossil in the center of the image surrounded by angular shells of fossil mytilids (clams commonly called mussels today). In life the mytilids had attached to the gastropod and each other by fine yet strong byssal thread produced by a special gland. This kind of relationship is very common in tidal pools and other shallow areas where wave action is strong.

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I Have Plenty of Faults

MAKHTESH GADOL, ISRAEL–One of the goals of this trip to the Negev was to map and analyze a series of faults Wooster geology students and Yoav Avni have found during our five years of fieldwork in Makhtesh Gadol.  Our projects have all been stratigraphic and paleontological, and we need to understand the structural framework of these rocks before we can interpret their histories.  In turn the faults could only be assessed after the stratigraphy has been sorted out, which we have essentially done now.  Yoav and I were able then to examine these faults this week and place them on the map with some ideas about their dimensions and times of movement.  (“Yoav and I” means in this case that I watched Yoav do the real work!)

Vertical fault (at the hammer head) in the Matmor Formation, Makhtesh Gadol, Israel.

Vertical fault (at the hammer head) in the Matmor Formation, Makhtesh Gadol, Israel.

Most of the faults are vertical and more or less east-west trending.  After mapping them, the fun part was working out how much displacement took place and when.  For example, using a Lower Cretaceous laterite as a key horizon, we could tell on one segment of a fault that 6.5 meters of displacement was prior to laterite formation and 4.5 meters came after the laterite.  This could only be done after the stratigraphy of the Jurassic units under the laterite was described, which is Wooster’s contribution to this structural analysis.

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Jurassic Cryptic Marine Ecosystems

Note the curly worm tubes and borings made by another type of worm.  There are also tiny little sponges in this view, and even tinier brachiopods.  This is a "cryptic community", meaning it lived in a protected space, in this case on the underside of a coral colony just above the sea floor.  The study of cryptic marine communities and their evolution has been a speciality of the Wooster paleontology lab.  (Matmor Formation, Jurassic, Makhtesh Gadol.)

Note the curly worm tubes and borings made by another type of worm. There are also tiny little sponges in this view, and even tinier brachiopods. This is a "cryptic community", meaning it lived in a protected space, in this case on the underside of a coral colony just above the sea floor. The study of cryptic marine communities and their evolution has been a speciality of the Wooster paleontology lab. (Matmor Formation, Jurassic, Makhtesh Gadol.)

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Watched

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MAKHTESH GADOL, ISRAEL–Our primary field area on this trip is near Dimona, Israel.  Outside the town is a famous facility with domed buildings and a very well guarded fence, complete with cameras and razor wire.  My Israeli friends tell me that it is a top secret ice cream research complex.

Part of the security for the production of all this “ice cream” is a tethered blimp which rises high above the desert, presumably carrying loads of cameras and other remote sensing devices.  Today we saw it being slowly reeled out, first rising as a startling image on the horizon of the makhtesh, and then almost disappearing in the distant sky.  We waved hello.

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“I Know a Tree …”

MAKHTESH GADOL, ISRAEL–Shade of any kind is rare in the Negev Desert, especially from trees.  At lunchtime in the field we want very much to be out of the sun, so usually someone suggests a lonely tree they know along a road or up some path.  The favorite tree for many Wooster geologists working in Makhtesh Gadol is the acacia pictured below.  Sure we’ve had to endure the camel flies and other camel offerings, but that shade has been heavenly.

One of the very few trees in Makhtesh Gadol.  This is an acacia.

One of the very few trees in Makhtesh Gadol. This is an acacia.

The acacias in the Negev are critical to animal ecosystems as well as in human ecology.  They are of a species which originated in Africa and migrated north into the Middle East.  They are genetically programmed to produce greenery and flowers during the African  monsoons in the summer.  As a consequence they are the only green and productive plants in the dry Negev summers, sustaining many animals with their leaves, flowers and beans.  The Bedouin Arabs depend on the acacia to feed their livestock during the hot and dry months in Israel and the surrounding countries.  Geologists are grateful for the high spreading branches which make a natural desert umbrella.

Leaves and flowers of the acacia tree shown above (left); beans and their pods on the ground beneath the tree.

Leaves and flowers of the acacia tree shown above (left); beans and their pods on the ground beneath the tree.

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