_version_ 1867167665743724544
author Monien, Patrick
Schnetger, Bernhard
Brumsack, Hans-Jürgen
Hass, H Christian
Kuhn, Gerhard
author_facet Monien, Patrick
Schnetger, Bernhard
Brumsack, Hans-Jürgen
Hass, H Christian
Kuhn, Gerhard
collection Datos científicos de ciencias marinas y ambientales
contents During RV Polarstern cruise ANT-XXIII/4 in 2006, a gravity core (PS69/335-2) and a giant box core (PS69/335-1) were retrieved from Maxwell Bay off King George Island (KGI). Comprehensive geochemical (bulk parameters, quantitative XRF, Inductively Coupled Plasma Mass Spectrometry) and radiometric dating analyses (14C, 210Pb) were performed on both cores. A comparison with geochemical data from local bedrock demonstrates a mostly detrital origin for the sediments, but also points to an overprint from changing bioproductivity in the overlying water column in addition to early diagenetic processes. Furthermore, ten tephra layers that were most probably derived from volcanic activity on Deception Island were identified. Variations in the vertical distribution of selected elements in Maxwell Bay sediments further indicate a shift in source rock provenance as a result of changing glacier extents during the past c. 1750 years that may be linked to the Little Ice Age and the Medieval Warm Period. Whereas no evidence for a significant increase in chemical weathering rates was found, 210Pb data revealed that mass accumulation rates in Maxwell Bay have almost tripled since the 1940s (0.66 g cm-2 yr-1 in AD 2006), which is probably linked to rapid glacier retreat in this region due to recent warming.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_759993
institution PANGAEA
language en
publishDate 2011
publisher PANGAEA
record_format pangaea
spellingShingle Geochemistry on sediment profile PS69/335
Monien, Patrick
Schnetger, Bernhard
Brumsack, Hans-Jürgen
Hass, H Christian
Kuhn, Gerhard
ANT-XXIII/4; GC; Giant box corer; GKG; Gravity corer; IMCOAST/IMCONet; Impact of climate induced glacier melt on marine coastal systems, Antarctica; Polarstern; Potter Cove, King George Island, Antarctic Peninsula; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; PS69; PS69/335-1; PS69/335-2; SPP1158
During RV Polarstern cruise ANT-XXIII/4 in 2006, a gravity core (PS69/335-2) and a giant box core (PS69/335-1) were retrieved from Maxwell Bay off King George Island (KGI). Comprehensive geochemical (bulk parameters, quantitative XRF, Inductively Coupled Plasma Mass Spectrometry) and radiometric dating analyses (14C, 210Pb) were performed on both cores. A comparison with geochemical data from local bedrock demonstrates a mostly detrital origin for the sediments, but also points to an overprint from changing bioproductivity in the overlying water column in addition to early diagenetic processes. Furthermore, ten tephra layers that were most probably derived from volcanic activity on Deception Island were identified. Variations in the vertical distribution of selected elements in Maxwell Bay sediments further indicate a shift in source rock provenance as a result of changing glacier extents during the past c. 1750 years that may be linked to the Little Ice Age and the Medieval Warm Period. Whereas no evidence for a significant increase in chemical weathering rates was found, 210Pb data revealed that mass accumulation rates in Maxwell Bay have almost tripled since the 1940s (0.66 g cm-2 yr-1 in AD 2006), which is probably linked to rapid glacier retreat in this region due to recent warming.
title Geochemistry on sediment profile PS69/335
topic ANT-XXIII/4; GC; Giant box corer; GKG; Gravity corer; IMCOAST/IMCONet; Impact of climate induced glacier melt on marine coastal systems, Antarctica; Polarstern; Potter Cove, King George Island, Antarctic Peninsula; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; PS69; PS69/335-1; PS69/335-2; SPP1158
url https://doi.org/10.1594/PANGAEA.759993