Oxygen isotopes, Mg/Ca ratios, sea surface temperature and counting of G. ruber morphotypes of sediment core MD01-2390
Cobertura |
LATITUDE: 6.635300 * LONGITUDE: 113.409000 * DATE/TIME START: 2001-05-18T06:40:00 * DATE/TIME END: 2001-05-18T06:40:00 * MINIMUM DEPTH, sediment/rock: 0.125 m * MAXIMUM DEPTH, sediment/rock: 8.825 m |
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Data(s) |
08/04/2006
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Formato |
text/tab-separated-values, 814 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.329730 doi:10.1594/PANGAEA.329730 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.738282 Steinke, Stephan; Chiu, Han-Yi; Yu, Pai-Sen; Shen, Chuan Chou; Erlenkeuser, Helmut; Löwemark, Ludvig; Chen, Min-Te (2006): On the influence of sea level and monsoon climate on the southern South China Sea freshwater budget over the last 22,000 years. Quaternary Science Reviews, 25(13-14), 1475-1488, doi:10.1016/j.quascirev.2005.12.008 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #AGE; Calculated; Comment; Counting >150 µm fraction; delta 18O, water; DEPTH, sediment/rock; Fragmentation index, planktic foraminifera; Giant piston corer; Globigerinoides ruber white; Globigerinoides ruber white, d18O; GPC; ICP-MS, Inductively coupled plasma - mass spectrometry; IMAGES; IMAGES VII - WEPAMA; International Marine Global Change Study; Magnesium/Calcium ratio; Marion Dufresne; Mass spectrometer Finnigan MAT 251; MD012390; MD01-2390; MD122; Planktic Foraminifers; Pteropoda; Sea surface temperature, annual mean; South China Sea |
Tipo |
Dataset |