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Scientific Drilling The open-access ICDP and IODP journal

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Sci. Dril., 16, 21-31, 2013
http://www.sci-dril.net/16/21/2013/
doi:10.5194/sd-16-21-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Science report
05 Nov 2013
Bighorn Basin Coring Project (BBCP): a continental perspective on early Paleogene hyperthermals
W. C. Clyde1, P. D. Gingerich2, S. L. Wing3, U. Röhl4, T. Westerhold4, G. Bowen5, K. Johnson6, A. A. Baczynski7, A. Diefendorf8, F. McInerney9, D. Schnurrenberger1, A. Noren10, K. Brady10, and the BBCP Science Team 1Department of Earth Sciences, University of New Hampshire, 56 College Rd., Durham, NH 03824, USA
2Department of Earth and Environmental Sciences and Museum of Paleontology, University of Michigan, Ann Arbor, MI 48109, USA
3Department of Paleobiology, Smithsonian Museum of Natural History, 10th Street and Constitution Avenue, NW, Washington, DC 20560, USA
4MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany
5Department of Geology & Geophysics, University of Utah, Salt Lake City, UT 84112, USA
6Smithsonian Museum of Natural History, 10th Street and Constitution Avenue, NW, Washington, DC 20560, USA
7Department of Earth and Planetary Sciences, Northwestern University, Evanston, IL 60208, USA
8Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA
9School of Earth & Environmental Sciences, University of Adelaide 5005, Australia
10LacCore, University of Minnesota, Minneapolis, MN 55455, USA
Abstract. During the summer of 2011, the Bighorn Basin Coring Project (BBCP) recovered over 900 m of overlapping core from 3 different sites in late Paleocene to early Eocene fluvial deposits of northwestern Wyoming. BBCP cores are being used to develop high-resolution proxy records of the Paleocene–Eocene Thermal Maximum (PETM) and Eocene Thermal Maximum 2 (ETM2) hyperthermal events. These events are short-term, large magnitude global warming events associated with extreme perturbations to the earth's carbon cycle. Although the PETM and ETM2 occurred ~55–52 million years ago, they are analogous in many ways to modern anthropogenic changes to the carbon cycle. By applying various sedimentological, geochemical, and palynological methods to the cores, we hope to better understand what caused these events, study the biogeochemical and ecological feedbacks that operated during them, and reveal precisely how they impacted continental environments.

Core recovery was >98% in all holes and most drilling was carried out without fluid additives, showing that continuous coring of continental smectitic deposits like these can be achieved with minimal risk of contamination to molecular biomarkers. Cores were processed in the Bremen Core Repository where the science team convened for 17 days to carry out data collection and sampling protocols similar to IODP projects. Initial results show that the weathered horizon extends to as much as ~30 m below the surface and variations in magnetic susceptibility within the cores record an interplay between grain size and pedogenesis. Previous investigations of outcrops near the BBCP drill sites allow detailed evaluation of the effects of weathering on common proxy methods. Studies of lithofacies, organic geochemistry, stable isotope geochemistry, calibrated XRF core scanning, paleomagnetics, and palynology are underway and will represent the highest resolution and most integrated proxy records of the PETM from a continental setting yet known. An extensive outreach program is in place to capitalize on the educational value associated with the Bighorn Basin's unusually complete record of Phanerozoic earth history.


Citation: Clyde, W. C., Gingerich, P. D., Wing, S. L., Röhl, U., Westerhold, T., Bowen, G., Johnson, K., Baczynski, A. A., Diefendorf, A., McInerney, F., Schnurrenberger, D., Noren, A., Brady, K., and the BBCP Science Team: Bighorn Basin Coring Project (BBCP): a continental perspective on early Paleogene hyperthermals, Sci. Dril., 16, 21-31, doi:10.5194/sd-16-21-2013, 2013.
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