(Table 2) Stable oxygen isotope ratios of Globigerinoides ruber and paleotemperature reconstruction of ODP Site 133-811 in the western Coral Sea off northeast Australia
| Cobertura |
LATITUDE: -16.515000 * LONGITUDE: 148.158000 * DATE/TIME START: 1990-08-17T00:00:00 * DATE/TIME END: 1990-08-20T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.04 m * MAXIMUM DEPTH, sediment/rock: 187.10 m |
|---|---|
| Data(s) |
09/09/1996
|
| Formato |
text/tab-separated-values, 570 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.703198 doi:10.1594/PANGAEA.703198 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.703203 Isern, Alexandra R; McKenzie, Judith A; Feary, David A (1996): The role of sea-surface temperature as a control on carbonate platform development in the western Coral Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 124(3-4), 247-272, doi:10.1016/0031-0182(96)80502-5 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #133-811; AGE; Calculated; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; Coral Sea; DEPTH, sediment/rock; Globigerinoides ruber white, d18O; Joides Resolution; Leg133; Mass spectrometer VG Isogas Prism; Ocean Drilling Program; ODP; Sea surface temperature, annual mean |
| Tipo |
Dataset |
