Antarctic Holocene climate change: A benthic foraminiferal stable isotope record from Palmer Deep

The first moderate- to high-resolution Holocene marine stable isotope record from the nearshore Antarctic continental shelf (Ocean Drilling Program (ODP) Hole 1098B) suggests sensitivity of the western Antarctic Peninsula hydrography to westerly wind strength and El Nino-Southern Oscillation (ENSO)-...

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Bibliographic Details
Main Authors: Shevenell, AE, Kennett, JP
Format: Article in Journal/Newspaper
Language:English
Published: AMER GEOPHYSICAL UNION 2002
Subjects:
Antarctic paleoceanography
Stable isotopes
Holocene
Climate change
Benthic foraminifera
Peninsula continental-shelf
Greenland ice-core
Southern-ocean
Sea-ice
North-Atlantic
Last deglaciation
Warm period
Ross sea
El-Nino
Variability
Antarctic
Southern Ocean
Antarctic Peninsula
Ross Sea
Greenland
Pacific
Palmer Deep
Antarc*
Greenland ice core
ice core
North Atlantic
Sea ice
Online Access:https://discovery.ucl.ac.uk/id/eprint/11203/1/2000PA000596.pdf
https://discovery.ucl.ac.uk/id/eprint/11203/
Description
Summary:The first moderate- to high-resolution Holocene marine stable isotope record from the nearshore Antarctic continental shelf (Ocean Drilling Program (ODP) Hole 1098B) suggests sensitivity of the western Antarctic Peninsula hydrography to westerly wind strength and El Nino-Southern Oscillation (ENSO)-like climate variability. Despite proximity to corrosive Antarctic water masses, sufficient CaCO3 in Palmer Deep sediments exists to provide a high-quality stable isotopic record (especially in the late Holocene). Coherence of benthic foraminifer delta(18)O, delta(13)C, sedimentologic, and CaCO3 fluctuations suggests that rapid (<20 years) Palmer Deep bottom water temperature fluctuations of 1&DEG;-1.5&DEG;C are associated with competitive interactions between two dominant oceanographic/climatic states. An abrupt shift from a warmer, stable Upper Circumpolar Deep Water (UCDW) state to a cooler, variable shelf water state occurred at &SIM;3.6 ka. Palmer Deep bottom waters oscillated between UCDW and shelf water-dominated states between &SIM;3.6 and 0.05 ka. Cool shelf water intervals correlate with Neoglacial events, the most recent and largest being the Little Ice Age (LIA; &SIM;0.7-0.2 ka). Similarities between Palmer Deep and global Holocene records and the rapidity of inferred bottom water fluctuations suggest that western Antarctic Peninsula shelf hydrography has not been controlled by thermohaline reorganizations but by variable strength and/or position of the Southern Hemisphere westerly wind field. We suggest that these atmospheric perturbations may have originated in the low-latitude tropical Pacific.

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