Stable carbon record and paleomagnetic of sediment core V28-179
| Cobertura |
LATITUDE: 4.617000 * LONGITUDE: -139.600000 * DATE/TIME START: 1971-02-25T00:00:00 * DATE/TIME END: 1971-02-25T00:00:00 |
|---|---|
| Data(s) |
18/02/1977
|
| Resumo |
Oxygen isotope and palaeomagnetic analysis of the lower half of LDGO piston core V28-179 shows that glacial-interglacial fluctuations have characterised Eart's climate for the past 3.2 Myr, before shich there was a period of stable 'interglacial' or 'preglacial' climate. The scale of glaciations increased about 2.5 Myr ago. |
| Formato |
application/zip, 2 datasets |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.733937 doi:10.1594/PANGAEA.733937 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Shackleton, Nicholas J; Opdyke, Neil D (1977): Oxygen isotope and palaeomagnetic evidence for early Northern Hemisphere glaciation. Nature, 270, 216-219, doi:10.1038/270216a0 |
| Palavras-Chave | #Datum level; Depth; DEPTH, sediment/rock; DL; G. subglobosa d13C; G. subglobosa d18O; Globocassidulina subglobosa, d13C; Globocassidulina subglobosa, d18O; Mass spectrometer VG Micromass 602; PC; Piston corer; Standard deviation; Std dev; V28; V28-179; Vema |
| Tipo |
Dataset |
