(Table 1) Upper Carboniferous spores abundances from ODP Holes 172-1062B, 172-1063A and 172-1063B
Cobertura |
MEDIAN LATITUDE: 31.873220 * MEDIAN LONGITUDE: -63.212293 * SOUTH-BOUND LATITUDE: 28.246470 * WEST-BOUND LONGITUDE: -74.407000 * NORTH-BOUND LATITUDE: 33.686720 * EAST-BOUND LONGITUDE: -57.614940 * DATE/TIME START: 1997-03-15T23:45:00 * DATE/TIME END: 1997-03-31T02:10:00 * MINIMUM ELEVATION: -4763.0 m * MAXIMUM ELEVATION: -4583.0 m |
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Data(s) |
23/08/2002
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Resumo |
Color variations were interpreted in paleoceanographic terms for the late Pliocene-Pleistocene sediments recovered by ODP Leg 172 on deep-sea drifts at Blake-Bahama Outer Ridge and northeastern Bermuda Rise. The color-derived parameters used in interpretation included predicted carbonate content, terrigenous fluxes, and hematite content. Abundance of Upper Carboniferous spores indicates that the hematite is probably derived from the Permo-Carboniferous red beds of the Canadian Maritimes. In the last 800 kyr sedimentation pattern changes on the Blake-Bahama Outer Ridge were determined by the sediment delivery to the deep basin as well as circulation changes. Sediment delivery increased during glacials (especially during the last 500 kyr and particularly since Stage 6). A fundamental change in the thermohaline circulation occurred at about 500 ka corresponding to the end of the Mid-Pleistocene Transition period at the onset of the predominant 100-kyr climate cyclicity. Sedimentation related to WBUC had intensified at that time and had become more focused at depths below 3000 m. Changes in hematite content and sedimentation rate show a pulse of sediment via the St. Lawrence outlet at the Pliocene-Pleistocene boundary suggesting that a likely change in the hydrography/physiography of the Laurentide Ice Sheet could have been involved in the climatic and ocean circulation changes at that time. |
Formato |
text/tab-separated-values, 126 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.764310 doi:10.1594/PANGAEA.764310 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Supplement to: Giosan, Liviu; Flood, Roger D; Grützner, Jens; Mudie, Peta J (2002): Paleoceanographic significance of sediment color on western North Atlantic Drifts: II. Late Pliocene-Pleistocene sedimentation. Marine Geology, 189(1-2), 43-61, doi:10.1016/S0025-3227(02)00322-5 |
Palavras-Chave | #172-1062B; 172-1063A; 172-1063B; Age, maximum/old; Age, minimum/young; Apiculatisporis; Blake-Bahama Outer Ridge, North Atlantic Ocean; Color description; Converrucosisporites; Counting, palynology; Densosporites; DRILL; Drilling/drill rig; Event label; Florinites; Joides Resolution; Laevigatosporites; Leg172; Leiotriletes; Lophotriletes; Lycospora; Murospora; Ocean Drilling Program; ODP; ODP sample designation; Punctatisporites; Sample code/label; Smear slide analysis; Spores indeterminata; Total counts; Triquitrites; Verrucosisporites |
Tipo |
Dataset |