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Microplankton abundance in the euphotic zone of the Aegean, Levantine and Ion...
Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger... -
Microplankton abundance in the euphotic zone of the Levantine Sea in October-...
Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger... -
Microplankton abundance in the euphotic zone of the Ionian Sea in October-Nov...
Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger... -
Microplankton abundance in the euphotic zone of the Aegean Sea in October-Nov...
Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger... -
Microplankton abundance at Station MARCH-1998-GN36199804610MSB01 in the eupho...
Microplankton species composition analysis was performed according to the inverted microscope method of Utermoehl. Samples for identification and enumeration of larger... -
(Table 1) Calcareous nannofossil distribution at ODP Site 180-1109 from the S...
The paleoceanography of the Solomon Sea for the last 195,000 years was investigated, based on the observations of 21 taxonomic groups of calcareous nannofossils in 144 samples... -
Nannofossil abundance of Hole 58-445
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 58-443
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 58-442A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 60-459B
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 2) Nannoplankton counts from ODP Hole 194-1195A
Sediment depth is given in mbsf. Abbreviation: (G) = good; (A) = abundant, more than 10 specimens occurring per field; common (c) = 1-10 specimens per field; few (f) = 1... -
(Table 1) Distribution of calcareous nannofossils in ODP Hole 167-1017E sedim...
Ocean Drilling Program (ODP) Site 1017E (34°32.10'N, 121°6.43'W; 955.5 m water depth) is located on Santa Lucia Slope, ~50 km west of Point Arguello. The location of Hole 1017E,... -
Phytoplankton abundance at bottle station A3/66A
This dataset has no description
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Phytoplankton abundance at bottle station A1/52
This dataset has no description
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Epipelagic coccolithophores in the global oceans
Presence = 1, absence = 0. -
Calcareous nanofossils in late Pliocene sediments of ODP Site 162-982
Sediment depth is given in revised composite depth [rmcd], AGE after Lawrence et al. (2009, doi:10.1029/2008PA001669) -
(Table S2c) Nannofossil species richness in ODP Site 198-1209
Species richness based on range extrapolation, species abundance: X = present, r = inferred reworked, questionable identification or ambiguous rare occurrence, * = extrapolated... -
(Table S2b) Nannofossil species richness in the Wilson Lake section
Species richness based on range extrapolation, species abundance: X = present, r = inferred reworked, questionable identification or ambiguous rare occurrence, * = extrapolated... -
(Table S2a) Nannofossil species richness in the Bass River section
Species richness based on range extrapolation, species abundance: X = present, r = inferred reworked, questionable identification or ambiguous rare occurrence, * = extrapolated... -
Phytoplankton biomass during Professor Vodyanitskiy cruise PV4
This dataset has no description
