Demise of the planktic foraminifer genus Morozovella during the early eocene climatic optimum: New records from ODP Site 1258 (Demerara Rise, western equatorial Atlantic) and Site 1263 (Walvis Ridge, south Atlantic)

• Published in: Geosciences
• Main Authors: D'onofrio R., Luciani V., Dickens G. R., Wade B. S., Turner S. K.
• Other Authors: D'Onofrio, R., Luciani, V., Dickens, G. R., Wade, B. S., Turner, S. K.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2020
• Subjects: Atlantic Ocean; Bulk carbon isotope; Early Eocene Climatic Optimum; Morozovella decline; Morozovella test-size reduction; Paleobiogeography; Planktic foraminiferal changes; Planktonic foraminifera
• Online Access: http://hdl.handle.net/11392/2421160; https://doi.org/10.3390/geosciences10030088; https://www.mdpi.com/2076-3263/10/3/88/pdf?version=1584598850; https://www.mdpi.com/2076-3263/10/3/88

Here we present relative abundances of planktic foraminifera that span the Early Eocene Climatic Optimum (EECO) at Ocean Drilling Program (ODP) Site 1258 in the western equatorial Atlantic. The EECO (~53.3−49.1 Ma) represents peak Cenozoic warmth, probably related to high atmospheric CO2, and when planktic foraminifera, a dominant component of marine sediment, exhibit a major biotic response. Consistent with previous work, the relative abundance of the genus Morozovella, which dominated early Paleogene tropical-subtropical assemblages, markedly and permanently declined from a mean percentage of ~32% to less than ~7% at the beginning of the EECO. The distinct decrease in Morozovella abundance occurred at Site 1258 within ~20 kyr before a negative excursion in δ13C records known as the J event and which defines the beginning of EECO. Moreover, all morozovellid species except M. aragonensis dropped in abundance permanently at Site 1258, and this is related to a reduction in test-size. Comparing our data with that from other locations, the remarkable switch in planktonic foraminifera assemblages appears to have begun first with unfavourable environmental conditions near the Equator and then extended to higher latitudes. Several potential stressors may explain observations, including some combination of algal photosymbiont inhibition (bleaching), a sustained increase in temperature, or an extended decrease in pH.