200,000 years of monsoonal history recorded on the lower Bengal Fan , IODP Hole 354-U1452C

We conducted a multidisciplinary study to provide the stratigraphic and palaeoclimatic context of monsoonal rainfall dynamics and their responses to orbital forcing for the Bay of Bengal. Using sediment lightness we established an age model at orbital resolution for International Ocean Discovery Pro...

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Bibliographic Details
Main Authors: Weber, Michael E, Lantzsch, Hendrik, Dekens, Petra S, Das, Supriyo Kumar, Reilly, Brendan T, Martos, Yasmina M, Meyer-Jacob, Carsten, Agrahari, Sandip, Ekblad, Alf, Titschack, Jürgen, Holmes, Elisabeth, Wolfgramm, Philipp
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
354-U1452C
Bengal Fan
CDRILL
Core drilling
EXP354
Integrated Ocean Drilling Program / International Ocean Discovery Program
IODP
Joides Resolution
Antarctic
Indian
Antarc*
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.889300
https://doi.org/10.1594/PANGAEA.889300
Description
Summary:We conducted a multidisciplinary study to provide the stratigraphic and palaeoclimatic context of monsoonal rainfall dynamics and their responses to orbital forcing for the Bay of Bengal. Using sediment lightness we established an age model at orbital resolution for International Ocean Discovery Programme (IODP) Core U1452C-1H that covers the last 200 ka in the lower Bengal Fan. The low-resolution δ18O of G. sacculifer is consistent with global δ18O records, at least for major glacial-to-interglacial transitions. The variability of total organic carbon, total nitrogen, and the δ13C composition of organic matter indicate the marine origin of organic matter. Marine primary productivity likely increased during insolation minima, indicative for an enhanced NE monsoon during glacials and stadials. Pristine insolation forcing is also documented for wet-bulk density, red-green color variability, and grain-size variations, indicating that darker and coarser-grained material deposited at higher sedimentation rates during insolation minima. Stronger NE monsoon likely amplified ocean-atmosphere interactions over the Indian Ocean, leading to stronger upwelling through shoaling the thermocline, and higher delivery of sediment to the Bay of Bengal due to higher soil erosion on land. In addition, lower glacial and stadial sea levels as well as stronger westward surface circulation favored delivery of coarser-grained fluvial material to the lower Bengal Fan. At the same time the stronger NE monsoon might have increased the aeolian supply. Total inorganic carbon, the Ca/Ti ratio, and biogenic silica vary dominantly on obliquity frequencies, suggesting mobilization and transport of lithogenic material primarily during lowered sea levels and/or higher influence of the Northern Hemisphere westerlies on the dust transport from the Tibetan Plateau. The close resemblance of sediment lightness and the climate record of Antarctic ice cores over multiple glacial cycles indicate close relationship between high southern latitude and ...

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