Microfossil evidence for trophic changes during the Eocene-Oligocene transition in the South Atlantic (ODP Site 1263, Walvis Ridge)

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doi: 10.5194/cp-11-1249-2015
Author(s): Bordiga, M.; Henderiks, J.; Tori, F.; Monechi, S.; Fenero, R.; Legarda-Lisarri, A.; Thomas, E.
Author Affiliation(s): Primary:
Uppsala University, Department of Earth Sciences, Uppsala, Sweden
Other:
Universita di Firenze, Italy
Universidad de Zaragoza, Spain
Yale University, United States
Volume Title: Climate of the Past
Source: Climate of the Past, 11(9), p.1249-1270. Publisher: Copernicus, Katlenburg-Lindau, International. ISSN: 1814-9324
Note: In English. 147 refs.; illus., incl. 1 table, sketch map
Summary: The biotic response of calcareous nannoplankton to environmental and climatic changes during the Eocene-Oligocene transition was investigated at a high resolution at Ocean Drilling Program (ODP) Site 1263 (Walvis Ridge, southeast Atlantic Ocean) and compared with a lower-resolution benthic foraminiferal record. During this time interval, global climate, which had been warm under high levels of atmospheric CO2 (pCO2) during the Eocene, transitioned into the cooler climate of the Oligocene, at overall lower pCO2. At Site 1263, the absolute nannofossil abundance (coccoliths per gram of sediment; N g-1) and the mean coccolith size decreased distinctly after the E-O boundary (EOB; 33.89 Ma), mainly due to a sharp decline in abundance of large-sized Reticulofenestra and Dictyococcites, occurring within a time span of ∼ 47 kyr. Carbonate dissolution did not vary much across the EOB; thus, the decrease in abundance and size of nannofossils may reflect an overall decrease in their export production, which could have led to variations in the food availability for benthic foraminifers. The benthic foraminiferal assemblage data are consistent with a global decline in abundance of rectilinear species with complex apertures in the latest Eocene (∼ 34.5 Ma), potentially reflecting changes in the food source, i.e., phytoplankton. This was followed by a transient increased abundance of species indicative of seasonal delivery of food to the sea floor (Epistominella spp.; ∼ 33.9-33.4 Ma), with a short peak in overall food delivery at the EOB (buliminid taxa; ∼ 33.8 Ma). Increased abundance of Nuttallides umbonifera (at ∼ 33.3 Ma) indicates the presence of more corrosive bottom waters and possibly the combined arrival of less food at the sea floor after the second step of cooling (Step 2). The most important changes in the calcareous nannofossil and benthic communities occurred ∼ 120 kyr after the EOB. There was no major change in nannofossil abundance or assemblage composition at Site 1263 after Step 2 although benthic foraminifera indicate more corrosive bottom waters during this time. During the onset of latest-Eocene-earliest-Oligocene climate change, marine phytoplankton thus showed high sensitivity to fast-changing conditions as well as to a possibly enhanced, pulsed nutrient supply and to the crossing of a climatic threshold (e.g., pCO2 decline, high-latitude cooling and changes in ocean circulation).
Year of Publication: 2015
Research Program: ODP Ocean Drilling Program
Key Words: 08 Paleontology, General; 12 Stratigraphy, Historical Geology and Paleoecology; Algae; Assemblages; Atlantic Ocean; Benthic taxa; Biostratigraphy; Biota; Biozones; Bottom water; C-13/C-12; Carbon; Cenozoic; Climate change; Coccolithophoraceae; Communities; Eocene; Foraminifera; Indicators; Invertebrata; Isotopes; Leg 208; Marine environment; Microfossils; Nannofossils; Nutrients; ODP Site 1263; Ocean Drilling Program; Oligocene; Paleoecology; Paleoenvironment; Paleogene; Planktonic taxa; Plantae; Preservation; Principal components analysis; Productivity; Protista; Sample preparation; Size; South Atlantic; Species diversity; Stable isotopes; Statistical analysis; Stratigraphic boundary; Tertiary; Tests; Trophic analysis; Variations; Walvis Ridge
Coordinates: S290000 S270000 E0030000 E0013000
Record ID: 2016044116
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Copernicus Gesellschaft, Katlenburg-Lindau, Germany