A High‐Fidelity Benthic Stable Isotope Record of Late Cretaceous–Early Eocene Climate Change and Carbon‐Cycling

• Published in: Paleoceanography and Paleoclimatology
• Main Authors: Barnet, JSK, Littler, K, Westerhold, T, Kroon, D, Leng, M, Bailey, I, Rohl, U, Zachos, J
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union (AGU) / Wiley 2019
• Subjects: paleoclimate; paleoceanography; orbital forcing; Paleocene; Eocene; stable isotopes; North Atlantic
• Online Access: http://hdl.handle.net/10871/36983; https://doi.org/10.1029/2019PA003556

This is the final version. Available on open access from AGU via the DOI in this record The complete benthic δ13C and δ18O data set underpinning this manuscript, along with additional % coarse fraction data generated across the Dan‐C2 event and our compilation of published and recalibrated atmospheric pCO2 estimates, are archived in the PANGAEA database (https://doi.pangaea.de/10.1594/PANGAEA.884588). The Late Cretaceous–Early Paleogene is the most recent period in Earth history that experienced sustained global greenhouse warmth on multimillion year timescales. Yet, knowledge of ambient climate conditions and the complex interplay between various forcing mechanisms are still poorly constrained. Here we present a 14.75 million‐year‐long, high‐resolution, orbitally tuned record of paired climate change and carbon‐cycling for this enigmatic period (~67–52 Ma), which we compare to an up‐to‐date compilation of atmospheric pCO2 records. Our climate and carbon‐cycling records, which are the highest resolution stratigraphically complete records to be constructed from a single marine site in the Atlantic Ocean, feature all major transient warming events (termed “hyperthermals”) known from this time period. We identify eccentricity as the dominant pacemaker of climate and the carbon cycle throughout the Late Maastrichtian to Early Eocene, through the modulation of precession. On average, changes in the carbon cycle lagged changes in climate by ~23,000 years at the long eccentricity (405,000‐year) band, and by ~3,000–4,500 years at the short eccentricity (100,000‐year) band, suggesting that light carbon was released as a positive feedback to warming induced by orbital forcing. Our new record places all known hyperthermals of the Late Maastrichtian–Early Eocene into temporal context with regards to evolving ambient climate of the time. We constrain potential carbon cycle influences of Large Igneous Province volcanism associated with the Deccan Traps and North Atlantic Igneous Province, as well as the sensitivity of ...