Pollen abundance in ODP Site 123-765 (Table 1)
Cobertura |
LATITUDE: -15.976000 * LONGITUDE: 117.575200 * DATE/TIME START: 1988-09-08T02:30:00 * DATE/TIME END: 1988-09-22T10:30:00 * MINIMUM ELEVATION: -5728.0 m * MAXIMUM ELEVATION: -5728.0 m |
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Data(s) |
19/11/1992
|
Resumo |
Middle Miocene to Holocene pollen assemblages reveal a history of environmental change in northern Australia. Grass pollen appeared, but was rare, in the late Miocene and was consistently present throughout the Pliocene, but did not become abundant until the Pleistocene. Myrtaceae pollen, characteristic of late Cenozoic assemblages in eastern Australia, is poorly represented, and no unequivocal evidence of rain forest was found. |
Formato |
text/tab-separated-values, 880 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.729427 doi:10.1594/PANGAEA.729427 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Supplement to: McMinn, Andrew; Martin, Helene A (1992): Late Cenozoic pollen history from Site 765, eastern Indian Ocean. In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 421-427, doi:10.2973/odp.proc.sr.123.166.1992 |
Palavras-Chave | #123-765B; 123-765C; Acacia; Asteraceae; Casuarinaceae; Chenopodiaceae; Counting, palynology; Cyatheae; Dodonaea viscosa; DRILL; Drilling/drill rig; Epoch; Event label; Gyrostemonaceae; Haloragis; Joides Resolution; Laevigatosporites ovatus; Leg123; Myrtaceae; Ocean Drilling Program; ODP; ODP sample designation; Poaceae; Podocarpus spp.; Pollen and spores; Polypodiidites sp.; Restionaceae; Sample code/label; South Indian Ridge, South Indian Ocean; Tricolporites spp.; Tricolporopollenites spp. |
Tipo |
Dataset |