Late Quaternary sediment accumulation in the Baffin Bay
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
1987
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| _version_ | 1867169501429104640 |
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| author | Andrews, John T |
| author_facet | Andrews, John T |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Piston cores from fiords, shelf troughs, and the deep-sea off eastern Baffin Island, N.W.T., Canada, have been sampled for texture and detrital carbonate in the <2 mm fraction. The sediments consist primarily of silty clays usually containing <5% sand. Estimates are made for sediment accumulation (kg/m**2/ka) over the last ca. 10 ka. Three sets, of two cores each, lie on a fiord-shelf transect and thus define variations in sediment accumulation gradients. These continental margin data are compared with cruder estimates of Holocene sediment accumulation at three sites farther offshore in Baffin Bay, Davis Strait and the northern Labrador Sea. Minimum accumulation in a 2 ka interval was 200 kg/m2 with a maximum estimate of 8,800 kg/m2. Detrital carbonate accumulation varies between 0 and 1,300 kg/m**2. Median accumulation for a typical fiord-shelf-deep-sea transect over the last 10 ka have been 10,340, 3493 and 820 kg/m**2. At DSDP Leg, site 645 in central Baffin Bay, the sedimentation rate ranged between 40 and 130 m/Ma (ca. 400 and 1200 kg/m**2/2ka); that is, comparable with the Late Quaternary input into Baffin Bay. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_743338 |
| institution | PANGAEA |
| language | en |
| publishDate | 1987 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Late Quaternary sediment accumulation in the Baffin Bay Andrews, John T Baffin Bay; Baffin Shelf; HU75-58; HU76-40; HU77-156; HU77-159; HU78-24; HU78-37; HU82-05CL; HU82-13; HU82-SU5; Ocean Drilling Program; ODP; PC; Piston corer Piston cores from fiords, shelf troughs, and the deep-sea off eastern Baffin Island, N.W.T., Canada, have been sampled for texture and detrital carbonate in the <2 mm fraction. The sediments consist primarily of silty clays usually containing <5% sand. Estimates are made for sediment accumulation (kg/m**2/ka) over the last ca. 10 ka. Three sets, of two cores each, lie on a fiord-shelf transect and thus define variations in sediment accumulation gradients. These continental margin data are compared with cruder estimates of Holocene sediment accumulation at three sites farther offshore in Baffin Bay, Davis Strait and the northern Labrador Sea. Minimum accumulation in a 2 ka interval was 200 kg/m2 with a maximum estimate of 8,800 kg/m2. Detrital carbonate accumulation varies between 0 and 1,300 kg/m**2. Median accumulation for a typical fiord-shelf-deep-sea transect over the last 10 ka have been 10,340, 3493 and 820 kg/m**2. At DSDP Leg, site 645 in central Baffin Bay, the sedimentation rate ranged between 40 and 130 m/Ma (ca. 400 and 1200 kg/m**2/2ka); that is, comparable with the Late Quaternary input into Baffin Bay. |
| title | Late Quaternary sediment accumulation in the Baffin Bay |
| topic | Baffin Bay; Baffin Shelf; HU75-58; HU76-40; HU77-156; HU77-159; HU78-24; HU78-37; HU82-05CL; HU82-13; HU82-SU5; Ocean Drilling Program; ODP; PC; Piston corer |
| url | https://doi.org/10.1594/PANGAEA.743338 |