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Impacts of elevated CO2 on particulate and dissolved organic matter productio...
Response of phytoplankton to increasing CO2 in seawater in terms of physiology and ecology is key to predicting changes in marine ecosystems. However, responses of natural... -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) in the Wadd...
0 = not present / 1 = present -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) in the Wadd...
0 = not present / 1 = present -
Microfossil abundance of Hole 13-128
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 5) Stratigraphic occurrence of Quaternary diatoms in DSDP Site 87-584
Sediment depth is given in mbsf. <1 = presence of taxa. -
(Table 3) Stratigraphic occurrence of upper Quaternary diatoms in DSDP Site 8...
Sediment depth is given in mbsf. <1 = presence of taxa. -
(Table 2) Stratigraphic occurrence of upper Quaternary diatoms in DSDP Site 8...
Sediment depth is given in mbsf. <1 = presence of taxa. Diatom zone: Pseudoeunotia doliosus. -
(Table 1) Stratigraphic occurrence of Quaternary diatoms in DSDP Site 87-582
Sediment depth is given in mbsf. <1 = presence of taxa. Diatom zone: Pseudoeunotia doliosus. -
Phytoplankton abundance during Professor Vodyanitskiy cruise PV13
Phytoplankton samples were taken by bottles from different depths between 0 - 150 m with up to 2 replicates per depth horizon. Samples were concentrated by back filtration using... -
Phytoplankton biomass during Professor Vodyanitskiy cruise PV13
Phytoplankton samples were taken by bottles from different depths between 0 - 150 m with up to 2 replicates per depth horizon. Samples were concentrated by back filtration using... -
Phytoplankton abundance during Mikhail Lomonosov cruise ML47
Phytoplankton samples were taken by bottles from different depths between 0 - 150 m with up to 15 replicates per depth horizon. Samples were concentrated by back filtration... -
Phytoplankton biomass during Mikhail Lomonosov cruise ML47
Phytoplankton samples were taken by bottles from different depths between 0 - 150 m with up to 15 replicates per depth horizon. Samples were concentrated by back filtration... -
(Table 1) Stratigraphic occurrence of selected diatom species from ODP Hole 1...
species abundance: A = abundant, C = common, F = few, R = rare, - = not observed -
Diatom abundance of Hole 86-578
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 86-577
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 17-165A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 2) Stratigraphic distribution and relative abundances of selected diat...
Species abundance: R = rare; S = sparse; F = frequent; C = common; A = abundant; lower-case abundance designators are interpreted as reworked occurrences. -
Diatom abundance of Hole 27-262
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 36-330A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 36-329
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
