Shelf ecosystems along the US Atlantic Coastal Plain prior to and during the Paleocene-Eocene Thermal Maximum: insights into the stratigraphic architecture
Doubrawa, M.; Stassen, P.; Robinson, M.M.; Babila, T.L.; Zachos, J.C.; Speijer, R.P. (2022). Shelf ecosystems along the US Atlantic Coastal Plain prior to and during the Paleocene-Eocene Thermal Maximum: insights into the stratigraphic architecture. Paleoceanography and Paleoclimatology 37(10): e2022PA004475. https://dx.doi.org/10.1029/2022PA004475 In: Paleoceanography and Paleoclimatology. American Geophysical Union: Washington DC. ISSN 2572-4525; e-ISSN 2572-4525, more |  |
| Keywords | Foraminifera [WoRMS]
Marine/Coastal | | Author keywords | Paleocene-Eocene Thermal Maximum (PETM); pre-onset excursion (POE); shelf ecosystem; benthic foraminifera; South Dover Bridge; stratigraphy |
| Authors | | Top | - Doubrawa, M., more
- Stassen, P., more
- Robinson, M.M.
| - Babila, T.L.
- Zachos, J.C.
- Speijer, R.P., more
| |
| Abstract | The Paleocene-Eocene Thermal Maximum (PETM) is the most pronounced global warming event of the early Paleogene related to atmospheric CO2 increases. It is characterized by negative δ18O and δ13C excursions recorded in sedimentary archives and a transient disruption of the marine biosphere. Sites from the U.S. Atlantic Coastal Plain show an additional small, but distinct δ13C excursion below the onset of the PETM, coined the “pre-onset excursion” (POE), mimicking the PETM-forced environmental perturbations. This study focuses on the South Dover Bridge core in Maryland, where the Paleocene-Eocene transition is stratigraphically constrained by calcareous nannoplankton and stable isotope data, and in which the POE is well-expressed. The site was situated in a middle neritic marine shelf setting near a major outflow of the paleo-Potomac River system. We generated high-resolution benthic foraminiferal assemblage, stable isotope, trace-metal, grain-size and clay mineralogy data. The resulting stratigraphic subdivision of this Paleocene-Eocene transition is placed within a depth transect across the paleoshelf, highlighting that the PETM sequence is relatively expanded. The geochemical records provide detailed insights into the paleoenvironment, developing from a well-oxygenated water column in latest Paleocene to a PETM-ecosystem under severe biotic stress-conditions, with shifts in food supply and temperature, and under dysoxic bottom waters in a more river-dominated setting. Environmental changes started in the latest Paleocene and culminated atthe onset of the PETM, hinting to an intensifying trigger rather than to an instantaneous event at the Paleocene-Eocene boundary toppling the global system. |
|
