(Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205
Variations in Mg/Ca-based sea surface temperature and oxygen isotope ratio (d18O) of the surface water in the northern East China Sea (ECS) were reconstructed with high resolution during the last 18 kyr using planktic foraminifera. Millennial-scale variations between warmer, more saline surface wate...
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ftdatacite:10.1594/pangaea.831134 2023-05-15T17:31:33+02:00 (Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 Kubota, Yoshimi Kimoto, Katsunori Tada, Ryuji Oda, Hirokuni Yokoyama, Yusuke Matsuzaki, Hiroyuki 2010 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.831134 https://doi.pangaea.de/10.1594/PANGAEA.831134 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1029/2009pa001891 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Age, dated standard deviation Calendar age Age, minimum/young Age, maximum/old Calendar age, standard deviation Age, dated material Age, 14C AMS Age, 14C calibrated Dataset dataset Supplementary Dataset 2010 ftdatacite https://doi.org/10.1594/pangaea.831134 https://doi.org/10.1029/2009pa001891 2022-02-09T13:16:26Z Variations in Mg/Ca-based sea surface temperature and oxygen isotope ratio (d18O) of the surface water in the northern East China Sea (ECS) were reconstructed with high resolution during the last 18 kyr using planktic foraminifera. Millennial-scale variations between warmer, more saline surface water and cooler, less saline surface water were recognized during the early deglacial period and the Holocene, suggesting changes in the mixing ratio between the Kuroshio Water and the Changjiang Diluted Water. Stronger East Asian summer monsoon (EASM) precipitation events in south China are identified at 10.5, 8.8, 7.0, 5.3, 4.7, 2.9, 1.7, and 0.5 ka, based on sea surface salinity (SSS) records of the northern ECS. Weaker EASM precipitation events are also detected at 9.3, 8.3, 7.3, 6.0, 3.3, 2.3, 0.7, and 0.4 ka during the Holocene. These events agree with the maxima in d18O records of stalagmites from various parts of the Changjiang (Yangtze) River drainage. This agreement supports that our SSS record properly captures the millennial-scale dry (less EASM precipitation) events over the drainage basin of the Changjiang River during the Holocene. These dry events are also in good agreement with North Atlantic ice-rafted events, suggesting a teleconnection between North Atlantic climate and the EASM during the Holocene. Dataset North Atlantic DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Age, dated standard deviation Calendar age Age, minimum/young Age, maximum/old Calendar age, standard deviation Age, dated material Age, 14C AMS Age, 14C calibrated |
spellingShingle |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Age, dated standard deviation Calendar age Age, minimum/young Age, maximum/old Calendar age, standard deviation Age, dated material Age, 14C AMS Age, 14C calibrated Kubota, Yoshimi Kimoto, Katsunori Tada, Ryuji Oda, Hirokuni Yokoyama, Yusuke Matsuzaki, Hiroyuki (Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 |
topic_facet |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Age, dated standard deviation Calendar age Age, minimum/young Age, maximum/old Calendar age, standard deviation Age, dated material Age, 14C AMS Age, 14C calibrated |
description |
Variations in Mg/Ca-based sea surface temperature and oxygen isotope ratio (d18O) of the surface water in the northern East China Sea (ECS) were reconstructed with high resolution during the last 18 kyr using planktic foraminifera. Millennial-scale variations between warmer, more saline surface water and cooler, less saline surface water were recognized during the early deglacial period and the Holocene, suggesting changes in the mixing ratio between the Kuroshio Water and the Changjiang Diluted Water. Stronger East Asian summer monsoon (EASM) precipitation events in south China are identified at 10.5, 8.8, 7.0, 5.3, 4.7, 2.9, 1.7, and 0.5 ka, based on sea surface salinity (SSS) records of the northern ECS. Weaker EASM precipitation events are also detected at 9.3, 8.3, 7.3, 6.0, 3.3, 2.3, 0.7, and 0.4 ka during the Holocene. These events agree with the maxima in d18O records of stalagmites from various parts of the Changjiang (Yangtze) River drainage. This agreement supports that our SSS record properly captures the millennial-scale dry (less EASM precipitation) events over the drainage basin of the Changjiang River during the Holocene. These dry events are also in good agreement with North Atlantic ice-rafted events, suggesting a teleconnection between North Atlantic climate and the EASM during the Holocene. |
format |
Dataset |
author |
Kubota, Yoshimi Kimoto, Katsunori Tada, Ryuji Oda, Hirokuni Yokoyama, Yusuke Matsuzaki, Hiroyuki |
author_facet |
Kubota, Yoshimi Kimoto, Katsunori Tada, Ryuji Oda, Hirokuni Yokoyama, Yusuke Matsuzaki, Hiroyuki |
author_sort |
Kubota, Yoshimi |
title |
(Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 |
title_short |
(Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 |
title_full |
(Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 |
title_fullStr |
(Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 |
title_full_unstemmed |
(Table 1) Age determination of sediment core KY07-04-PC1, supplement to: Kubota, Yoshimi; Kimoto, Katsunori; Tada, Ryuji; Oda, Hirokuni; Yokoyama, Yusuke; Matsuzaki, Hiroyuki (2010): Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea. Paleoceanography, 25(4), PA4205 |
title_sort |
(table 1) age determination of sediment core ky07-04-pc1, supplement to: kubota, yoshimi; kimoto, katsunori; tada, ryuji; oda, hirokuni; yokoyama, yusuke; matsuzaki, hiroyuki (2010): variations of east asian summer monsoon since the last deglaciation based on mg/ca and oxygen isotope of planktic foraminifera in the northern east china sea. paleoceanography, 25(4), pa4205 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2010 |
url |
https://dx.doi.org/10.1594/pangaea.831134 https://doi.pangaea.de/10.1594/PANGAEA.831134 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1029/2009pa001891 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.831134 https://doi.org/10.1029/2009pa001891 |
_version_ |
1766129189234147328 |