Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ...
Most of the temperature reconstructions for the past two millennia are based on proxy data from various sites on land. Here we present a bidecadal resolution record of sea surface temperature (SST) in Southern Okinawa Trough for the past ca. 2700 years by analyzing tetraether lipids of planktonic ar...
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Online Access: | https://dx.doi.org/10.1594/pangaea.803648 https://doi.pangaea.de/10.1594/PANGAEA.803648 |
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ftdatacite:10.1594/pangaea.803648 2024-04-28T08:36:31+00:00 Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... Wu, Weichao Tan, Wenbing Zhou, Liping Yang, Huan Xu, Yunping 2012 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.803648 https://doi.pangaea.de/10.1594/PANGAEA.803648 en eng PANGAEA https://dx.doi.org/10.1029/2012gl052749 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Age Sea surface temperature Drilling/drill rig Calculated from TEX86 Kim et al., 2010 Leg195 Joides Resolution Ocean Drilling Program ODP dataset Dataset 2012 ftdatacite https://doi.org/10.1594/pangaea.80364810.1029/2012gl052749 2024-04-02T12:09:11Z Most of the temperature reconstructions for the past two millennia are based on proxy data from various sites on land. Here we present a bidecadal resolution record of sea surface temperature (SST) in Southern Okinawa Trough for the past ca. 2700 years by analyzing tetraether lipids of planktonic archaea in the ODP Hole 1202B, a site under the strong influence of Kuroshio Current and East Asian monsoon. The reconstructed SST anomalies generally coincided with previously reported late Holocene climate events, including the Roman Warm Period, Sui-Tang dynasty Warm Period, Medieval Warm Period, Current Warm Period, Dark Age Cold Period and Little Ice Age. However, the Medieval Warm Period usually thought to be a historical analogue for the Current Warm Period has a mean SST of 0.6-0.8°C lower than that of the Roman Warm Period and Sui-Tang dynasty Warm Period. Despite an increase since 1850 AD, the mean SST in the 20th century is still within the range of natural variability during the past 2700 years. A close ... : The chronology was established based on six 14C datings using planktonic foraminifera. Each sample was run in duplicate and the average standard deviation is 0.003, corresponding to 0.2 degree. The SST data in highlight is from the satellite derived mean annual SST (http://www.nsof.noaa.gov) ... Dataset Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Age Sea surface temperature Drilling/drill rig Calculated from TEX86 Kim et al., 2010 Leg195 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Age Sea surface temperature Drilling/drill rig Calculated from TEX86 Kim et al., 2010 Leg195 Joides Resolution Ocean Drilling Program ODP Wu, Weichao Tan, Wenbing Zhou, Liping Yang, Huan Xu, Yunping Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... |
topic_facet |
Age Sea surface temperature Drilling/drill rig Calculated from TEX86 Kim et al., 2010 Leg195 Joides Resolution Ocean Drilling Program ODP |
description |
Most of the temperature reconstructions for the past two millennia are based on proxy data from various sites on land. Here we present a bidecadal resolution record of sea surface temperature (SST) in Southern Okinawa Trough for the past ca. 2700 years by analyzing tetraether lipids of planktonic archaea in the ODP Hole 1202B, a site under the strong influence of Kuroshio Current and East Asian monsoon. The reconstructed SST anomalies generally coincided with previously reported late Holocene climate events, including the Roman Warm Period, Sui-Tang dynasty Warm Period, Medieval Warm Period, Current Warm Period, Dark Age Cold Period and Little Ice Age. However, the Medieval Warm Period usually thought to be a historical analogue for the Current Warm Period has a mean SST of 0.6-0.8°C lower than that of the Roman Warm Period and Sui-Tang dynasty Warm Period. Despite an increase since 1850 AD, the mean SST in the 20th century is still within the range of natural variability during the past 2700 years. A close ... : The chronology was established based on six 14C datings using planktonic foraminifera. Each sample was run in duplicate and the average standard deviation is 0.003, corresponding to 0.2 degree. The SST data in highlight is from the satellite derived mean annual SST (http://www.nsof.noaa.gov) ... |
format |
Dataset |
author |
Wu, Weichao Tan, Wenbing Zhou, Liping Yang, Huan Xu, Yunping |
author_facet |
Wu, Weichao Tan, Wenbing Zhou, Liping Yang, Huan Xu, Yunping |
author_sort |
Wu, Weichao |
title |
Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... |
title_short |
Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... |
title_full |
Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... |
title_fullStr |
Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... |
title_full_unstemmed |
Sea surface temperature oscillations in southern Okinawa Trough during last 2700 years from ODP Hole 195-1202B ... |
title_sort |
sea surface temperature oscillations in southern okinawa trough during last 2700 years from odp hole 195-1202b ... |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.803648 https://doi.pangaea.de/10.1594/PANGAEA.803648 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1029/2012gl052749 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.80364810.1029/2012gl052749 |
_version_ |
1797568272137191424 |