Foraminiferal Stable Isotope Record at Millville, NJ: Implications for the onset of the PETM
Abstract
Traditional paleoceanographic tools (magneto-biostratigraphy, orbital cycles) are insufficient to assign rates to the initial release of carbon during the rapid onset of the PETM (<10 kyr). The ODP Leg 174AX Millville, NJ PETM section (70 m paleodepth) is >10 times more expanded relative to the thickest open ocean sites (e.g., Site 690). The onset interval at Millville is defined by a bulk carbonate δ13C of 3.5‰ across 25 cm interval. Two groups used the geochemical changes to constrain the timing for the initial pulse of carbon. Wright and Schaller (2013) focused on the differential responses in δ13C and %CaCO3 arguing that the release was fast (<1 year). Conversely, Zeebe et al. (2016) assumed the initial covariance in δ18O and δ13C represented equilibrium conditions, modeling a 4 kyr duration for the release. We generated planktonic and benthic foraminiferal stable isotope records across the onset of the PETM CIE at Millville. Most of the δ13C change recorded by foraminifera occurred over the 25 cm onset interval. However, foraminiferal δ18O values continue to decrease for another 1.5 m above the initial δ13C decrease contradicting Zeebe et al.'s assumption of equilibrium conditions. The foraminiferal stable isotope pattern is similar to the modeled response following a large, instantaneous release of light carbon to the atmosphere, that produces a rapid (decadal) scale warming in the surface air masses followed by continued warming but at a slower rate. Differential responses in δ13C, δ18O, and %CaCO3 at the onset of the PETM are consistent with an instantaneous initial release of carbon with centennial-scale warming that continued well after the initial carbon pulse similar to that predicted by climate models. Fitting the Millville isotope records to these models suggests that peak warmth followed the initial release by 100 to 200 years. The mid-shelf location of Millville a made it responsive to atmospheric changes unlike open ocean sites where thermal inertia dampens the larger atmosphere changes.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2016
- Bibcode:
- 2016AGUFMPP51C2322W
- Keywords:
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- 0428 Carbon cycling;
- BIOGEOSCIENCESDE: 1051 Sedimentary geochemistry;
- GEOCHEMISTRYDE: 1605 Abrupt/rapid climate change;
- GLOBAL CHANGEDE: 4912 Biogeochemical cycles;
- processes;
- and modeling;
- PALEOCEANOGRAPHY