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(Table 2) Stratigraphic occurrences of Neogene diatoms in ODP Hole 127-794A
Sediment depth is given in mbsf, # indicates reworked specimens. -
(Table 1) Stratigraphic occurrences of Neogene diatoms in ODP Hole 127-797B
Sediment depth is given in mbsf, # indicates reworked specimens. -
(Table 3) Diatom abundances in ODP Hole 150-906A
Species abundance: A = abundnat, C = common, R = rare, -= absent. -
(Table 2) Diatom abundances in ODP Hole 150-903A
Species abundance: A = abundnat, C = common, R = rare, -= absent. -
(Table 8) Distribution of diatoms in Miocene to Pleistocene sediments of DSDP...
Species abundaces: D = dominant, A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 1) Occurrence of upper Pliocene to Quaternary diatom species and selec...
species abundance: A = abundant (at least 20 specimens are presented in one horizontal traverse at 500 X), C = common (19-3 specimens), F = few (1-2 specimens), R = rare (less... -
(Table 2) Composition, diversity, and abundance of diatoms in the surface sed...
Freshwater and brackish-water species: Achnanthes sp., Amphiprora sp., Asterionella formosa, Aulacosira granulata, Aulacosira islandica, Aulacosira italica, Aulacosira sp.,... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS7a_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS6_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS5_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS4_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS3_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS2_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
(Table 3) Relative abundance of key diatom taxa in sediments from DSDP Hole 6...
Counts were made at 500X, ignoring Chaetoceros spores and Thalassionema nitzschioides that dominate the sediment assemblages and mask subtle seasonal changes that occur in less... -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) - Wadden Se...
In order to monitor long-term variability in or eventual change of the planktonic community a semiquantitative analysis of microplankton based on net sampling is ongoing since... -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) - Wadden Se...
In order to monitor long-term variability in or eventual change of the planktonic community a semiquantitative analysis of microplankton based on net sampling is ongoing since... -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) - Wadden Se...
In order to monitor long-term variability in or eventual change of the planktonic community a semiquantitative analysis of microplankton based on net sampling is ongoing since... -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) - Wadden Se...
In order to monitor long-term variability in or eventual change of the planktonic community a semiquantitative analysis of microplankton based on net sampling is ongoing since... -
Diatom percentage abundances and sea surface temperature reconstruction for c...
Here, we present datasets of diatom abundance and a diatom-based sea surface temperature reconstruction from the Iceland Basin. The 419.5 cm long marine sediment core... -
Diatom percentage abundances and sea surface temperature reconstruction for c...
Due to the shortness of available records, the longterm patterns of climate variability in the Labrador Sea and Newfoundland region are not clear. Here, a diatom-based...