Geochemistry, sediment components, and paleoproductivity reconstruction for the Miocene to early Pliocene sediments ...

We reconstruct paleoproductivity at three sites in the Atlantic Ocean (Ocean Drilling Program Sites 982, 925, and 1088) to investigate the presence and extent of the late Miocene to early Pliocene 'biogenic bloom' from 9 to 3 Ma. Our approach involves construction of multiple records inclu...

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Bibliographic Details
Main Authors: Diester-Haass, Lieselotte, Billups, Katharina, Emeis, Kay-Christian
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2005
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.835306
https://doi.pangaea.de/10.1594/PANGAEA.835306
Description
Summary:We reconstruct paleoproductivity at three sites in the Atlantic Ocean (Ocean Drilling Program Sites 982, 925, and 1088) to investigate the presence and extent of the late Miocene to early Pliocene 'biogenic bloom' from 9 to 3 Ma. Our approach involves construction of multiple records including benthic foraminiferal and CaCO3 accumulation rates, Uvigerina counts, dissolution proxies, and geochemical tracers for biogenic and detrital fluxes. This time interval also contains the so-called late Miocene carbon isotope shift, a well-known decrease in benthic foraminiferal d13C values. We find that the timing of paleoproductivity maxima differs among the three sites. At Site 982 (North Atlantic), benthic foraminifera and CaCO3 accumulation were both at a maximum at ~5 Ma, with smaller peaks at ~6 Ma. The paleoproductivity maximum was centered earlier (~6.6-6.0 Ma) in the tropical Atlantic (Site 925). In the South Atlantic (Site 1088), paleoproductivity increased even earlier, between 8.2 Ma and 6.2 Ma, and remained ... : Supplement to: Diester-Haass, Lieselotte; Billups, Katharina; Emeis, Kay-Christian (2005): In search of the late Miocene-early Pliocene “biogenic bloom” in the Atlantic Ocean (Ocean Drilling Program Sites 982, 925, and 1088). Paleoceanography, 20(4), PA4001 ...