A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego
Situated at the southern margin of the hemispheric westerly wind belt and immediately north of the Antarctic Polar Frontal zone, Tierra del Fuego is well-positioned to monitor coupled changes in the ocean-atmosphere system of the high southern latitudes. Here we describe a Holocene paleoclimate reco...
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Online Access: | https://doi.org/10.1016/j.epsl.2010.11.011 |
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fteawag:oai:dora:eawag_6613 2024-09-15T17:48:20+00:00 A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego Moy, Christopher M. Dunbar, Robert B. Guilderson, Thomas P. Waldmann, Nicolas Mucciarone, David A. Recasens, Cristina Ariztegui, Daniel Austin Jr., James A. Anselmetti, Flavio S. 2011 https://doi.org/10.1016/j.epsl.2010.11.011 eng eng Elsevier Earth and Planetary Sciences Letters--Earth Planet. Sci. Lett.--journals:732--0012-821X--1385-013X eawag:6613 journal id: journals:732 issn: 0012-821X e-issn: 1385-013X ut: 000287555800001 local: 14835 scopus: 2-s2.0-78751584803 doi:10.1016/j.epsl.2010.11.011 Southern Hemisphere westerly winds Holocene paleoclimate radiocarbon stable isotopes Tierra del Fuego Text Journal Article 2011 fteawag https://doi.org/10.1016/j.epsl.2010.11.011 2024-08-05T03:04:28Z Situated at the southern margin of the hemispheric westerly wind belt and immediately north of the Antarctic Polar Frontal zone, Tierra del Fuego is well-positioned to monitor coupled changes in the ocean-atmosphere system of the high southern latitudes. Here we describe a Holocene paleoclimate record from sediment cores obtained from Lago Fagnano, a large lake in southern Tierra del Fuego at 55°S, to investigate past changes in climate related to these two important features of the global climate system. We use an AMS radiocarbon chronology for the last 8000yr based on pollen concentrates, thereby avoiding contamination from bedrock-derived lignite. Our chronology is consistent with a tephrochronologic age date for deposits from the middle Holocene Volcán Hudson eruption. Combining bulk organic isotopic (δ 13 C and δ 15 N) and elemental (C and N) parameters with physical sediment properties allows us to better understand sediment provenance and transport mechanisms and to interpret Holocene climate and tectonic change during the last 8000 yr. Co-variability and long-term trends in C/N ratio, carbon accumulation rate, and magnetic susceptibility reflect an overall Holocene increase in the delivery of terrestrial organic and lithogenic material to the deep eastern basin. We attribute this variability to westerly wind-derived precipitation. Increased wind strength and precipitation in the late Holocene drives the Nothofagus forest eastward and enhances run-off and terrigenous inputs to the lake. Superimposed on the long-term trend are a series of abrupt 9 negative departures in C/N ratio, which constrain the presence of seismically-driven mass flow events in the record. We identify an increase in bulk δ 13 C between 7000 and 5000 cal yr BP that we attribute to enhanced aquatic productivity driven by warmer summer temperatures. The Lago Fagnano δ 13 C record shows similarities with Holocene records of sea surface temperature from the mid-latitude Chilean continental shelf and Antarctic air temperatures from the ... Article in Journal/Newspaper Antarc* Antarctic Tierra del Fuego DORA Eawag Earth and Planetary Science Letters 302 1-2 1 13 |
institution |
Open Polar |
collection |
DORA Eawag |
op_collection_id |
fteawag |
language |
English |
topic |
Southern Hemisphere westerly winds Holocene paleoclimate radiocarbon stable isotopes Tierra del Fuego |
spellingShingle |
Southern Hemisphere westerly winds Holocene paleoclimate radiocarbon stable isotopes Tierra del Fuego Moy, Christopher M. Dunbar, Robert B. Guilderson, Thomas P. Waldmann, Nicolas Mucciarone, David A. Recasens, Cristina Ariztegui, Daniel Austin Jr., James A. Anselmetti, Flavio S. A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego |
topic_facet |
Southern Hemisphere westerly winds Holocene paleoclimate radiocarbon stable isotopes Tierra del Fuego |
description |
Situated at the southern margin of the hemispheric westerly wind belt and immediately north of the Antarctic Polar Frontal zone, Tierra del Fuego is well-positioned to monitor coupled changes in the ocean-atmosphere system of the high southern latitudes. Here we describe a Holocene paleoclimate record from sediment cores obtained from Lago Fagnano, a large lake in southern Tierra del Fuego at 55°S, to investigate past changes in climate related to these two important features of the global climate system. We use an AMS radiocarbon chronology for the last 8000yr based on pollen concentrates, thereby avoiding contamination from bedrock-derived lignite. Our chronology is consistent with a tephrochronologic age date for deposits from the middle Holocene Volcán Hudson eruption. Combining bulk organic isotopic (δ 13 C and δ 15 N) and elemental (C and N) parameters with physical sediment properties allows us to better understand sediment provenance and transport mechanisms and to interpret Holocene climate and tectonic change during the last 8000 yr. Co-variability and long-term trends in C/N ratio, carbon accumulation rate, and magnetic susceptibility reflect an overall Holocene increase in the delivery of terrestrial organic and lithogenic material to the deep eastern basin. We attribute this variability to westerly wind-derived precipitation. Increased wind strength and precipitation in the late Holocene drives the Nothofagus forest eastward and enhances run-off and terrigenous inputs to the lake. Superimposed on the long-term trend are a series of abrupt 9 negative departures in C/N ratio, which constrain the presence of seismically-driven mass flow events in the record. We identify an increase in bulk δ 13 C between 7000 and 5000 cal yr BP that we attribute to enhanced aquatic productivity driven by warmer summer temperatures. The Lago Fagnano δ 13 C record shows similarities with Holocene records of sea surface temperature from the mid-latitude Chilean continental shelf and Antarctic air temperatures from the ... |
format |
Article in Journal/Newspaper |
author |
Moy, Christopher M. Dunbar, Robert B. Guilderson, Thomas P. Waldmann, Nicolas Mucciarone, David A. Recasens, Cristina Ariztegui, Daniel Austin Jr., James A. Anselmetti, Flavio S. |
author_facet |
Moy, Christopher M. Dunbar, Robert B. Guilderson, Thomas P. Waldmann, Nicolas Mucciarone, David A. Recasens, Cristina Ariztegui, Daniel Austin Jr., James A. Anselmetti, Flavio S. |
author_sort |
Moy, Christopher M. |
title |
A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego |
title_short |
A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego |
title_full |
A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego |
title_fullStr |
A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego |
title_full_unstemmed |
A geochemical and sedimentary record of high southern latitude Holocene climate evolution from Lago Fagnano, Tierra del Fuego |
title_sort |
geochemical and sedimentary record of high southern latitude holocene climate evolution from lago fagnano, tierra del fuego |
publisher |
Elsevier |
publishDate |
2011 |
url |
https://doi.org/10.1016/j.epsl.2010.11.011 |
genre |
Antarc* Antarctic Tierra del Fuego |
genre_facet |
Antarc* Antarctic Tierra del Fuego |
op_relation |
Earth and Planetary Sciences Letters--Earth Planet. Sci. Lett.--journals:732--0012-821X--1385-013X eawag:6613 journal id: journals:732 issn: 0012-821X e-issn: 1385-013X ut: 000287555800001 local: 14835 scopus: 2-s2.0-78751584803 doi:10.1016/j.epsl.2010.11.011 |
op_doi |
https://doi.org/10.1016/j.epsl.2010.11.011 |
container_title |
Earth and Planetary Science Letters |
container_volume |
302 |
container_issue |
1-2 |
container_start_page |
1 |
op_container_end_page |
13 |
_version_ |
1810289475788472320 |