Dunkley Jones, T;
Major shifts in calcareous phytoplankton assemblages through the Eocene-Oligocene transition of Tanzania and their implications for low-latitude primary production.
, Article PA4204. 10.1029/2008PA001640.
Available under License : See the attached licence file.
A high-resolution record of exceptionally well preserved calcareous nannofossil assemblages from Tanzania is marked by two key transitions closely related to the climatic events of the Eocene-Oligocene transition (EOT). The first transition, at similar to 34.0 Ma, precedes the first positive shift in delta O-18 and coincides with a distinct interval of very low nannofossil abundance and a cooling in sea surface temperatures (SST). The second, at similar to 33.63 Ma, is immediately above the Eocene-Oligocene boundary (EOB) and is associated with a significant drop in nannofossil diversity. Both transitions involve significant reductions in the abundance of holococcoliths and other oligotrophic taxa. These changes in calcareous phytoplankton assemblages indicate (1) a widespread and significant perturbation to the low-latitude surface ocean closely tied to the EOB, (2) a potential role for reduced carbonate primary production at the onset of global cooling, and (3) a significant increase in nutrient availability in the low-latitude surface ocean through the EOT.
|Title:||Major shifts in calcareous phytoplankton assemblages through the Eocene-Oligocene transition of Tanzania and their implications for low-latitude primary production|
|Open access status:||An open access version is available from UCL Discovery|
|Additional information:||Copyright 2008 by the American Geophysical Union|
|Keywords:||Indian-ocean, Atlantic-ocean, Eocene/oligocene boundary, Antarctic glaciation, Earliest oligocene, Coastal Tanzania, Thermal maximum, Stable-isotope, Climate-change, Nannofossil assemblages|
|UCL classification:||UCL > School of BEAMS
UCL > School of BEAMS > Faculty of Maths and Physical Sciences
UCL > School of Arts and Social Sciences
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