Data from: Calcareous nannoplankton ecology and community change across the Paleocene-Eocene Thermal Maximum

• Main Authors: Schneider, Leah J., Bralower, Timothy J., Kump, Lee R., Patzkowsky, Mark E.
• Format: Dataset
• Language: unknown
• Published: Data Archiving and Networked Services (DANS) 2013
• Subjects: Life sciences; medicine and health care; Zygodiscus; Zygrhablithus; Cruciplacolithus; Ellipsolithus; Paleocene; Pontosphaera; Coccolithus; Neochiastozygus; PETM; Biscutum; Toweius; Sphenolithus; Camplyosphaera; calcareous nannoplankton; Coronocyclus; Eocene; Zeugrhabdotus; climate; Hornibrookina; Prinsius; Discoaster; Fasciculithus; Rhomboaster; Paleoecology; Chiasmolithus; Thoracosphaera; Neococcolithes; Octolithus; micropaleontology; Ericsonia; Calciosolenia; New Jersey Shelf; Tethys; North Atlantic; South Atlantic; Southern Ocean; North Pacific; geo; envir; Pacific
• Online Access: https://doi.org/10.5061/dryad.m05c8

The Paleocene-Eocene Thermal Maximum (PETM; ca. 55.8 Ma) is thought to coincide with a profound but entirely transient change among nannoplankton communities throughout the ocean. Here we explore the ecology of nannoplankton during the PETM by using multivariate analyses of a global data set that is based upon the distribution of taxa in time and space. We use these results, coupled with stable isotope data and geochemical modeling, to reinterpret the ecology of key genera. The results of the multivariate analyses suggest that the community was perturbed significantly in coastal and high- latitudes sites compared to the open ocean, and the relative influence of temperature and nutrient availability on the assemblage varies regionally. The open ocean became more stratified and less productive during the PETM and the oligotrophic assemblage responded primarily to changes in nutrient availability. Alternatively, assemblages at the equator and in the Southern Ocean responded to temperature more than to nutrient reduction. In addition, the assemblage change at the PETM was not merely transient-there is evidence of adaptation and a long-term change in the nannoplankton community that persists after the PETM and results in the disappearance of a high- latitude assemblage. The long-term effect on communities caused by transient warming during the PETM has implications for modern- day climate change, suggesting similar permanent changes to nannoplankton community structure as the oceans warm. Supplementary Table 1Detrended correspondence analysis (DCA) values of axes 1-4 for calcareous nannofossil genera and localities across the Paleocene-Eocene Thermal Maximum (PETM). The DCA was created using the 'decorana' function in the program R. For more information on the statistical methods, see the associated manuscript. The locality name and the Ocean Drilling Program (ODP) Site number (if applicable) are given as well as the depth of the sample. The sample depths for Forada, Italy have both positive and negative values, ...