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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... -
(Table T5) Stratigraphic occurence and relative abundances of diatom taxa fro...
Abundance: D = dominant >60%, A = abundant 30-60, C = common 15-30, F = few 3-15, R = rare <3, T = trace, X = present, - = none. Preservation: G = good, M = moderate, P =... -
(Table T4) Stratigraphic occurence and relative abundances of diatom taxa fro...
Abundance: D = dominant >60%, A = abundant 30-60, C = common 15-30, F = few 3-15, R = rare <3, T = trace, X = present, - = none. Preservation: G = good, M = moderate, P =... -
(Table T3) Stratigraphic occurence and relative abundances of diatom taxa fro...
Abundance: D = dominant >60%, A = abundant 30-60, C = common 15-30, F = few 3-15, R = rare <3, T = trace, X = present, - = none. Preservation: G = good, M = moderate, P =... -
(Table T2) Stratigraphic occurence and relative abundances of diatom taxa fro...
Abundance: D = dominant >60%, A = abundant 30-60, C = common 15-30, F = few 3-15, R = rare <3, T = trace, X = present, - = none. Preservation: G = good, M = moderate, P =... -
(Table T1) Stratigraphic occurence and relative abundances of diatom taxa fro...
Abundance: D = dominant >60%, A = abundant 30-60, C = common 15-30, F = few 3-15, R = rare <3, T = trace, X = present, - = none. Preservation: G = good, M = moderate, P =... -
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 -
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) -
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... -
Phytoplankton biomass during Professor Vodyanitskiy cruise PV23
This dataset has no description
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Phytoplankton biomass during Professor Vodyanitskiy cruise PV4
This dataset has no description
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Phytoplankton abundance during Professor Vodyanitskiy cruise PV23
This dataset has no description
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Phytoplankton abundance during Professor Vodyanitskiy cruise PV4
This dataset has no description
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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.
