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Phytoplankton long-term time-series at the fixed coastal station in the Gulf ...
Identification and counts of specimens were performed at the inverted microscope after sedimentation of variable volumes of seawater (1-100 ml), depending on cell concentration... -
Phytoplankton long-term time-series at the fixed coastal station in the Gulf ...
Identification and counts of specimens were performed at the inverted microscope after sedimentation of variable volumes of seawater (1-100 ml), depending on cell concentration... -
Phytoplankton long-term time-series at the fixed coastal station in the Gulf ...
Identification and counts of specimens were performed at the inverted microscope after sedimentation of variable volumes of seawater (1-100 ml), depending on cell concentration... -
Phytoplankton long-term time-series at the fixed coastal station in the Gulf ...
Identification and counts of specimens were performed at the inverted microscope after sedimentation of variable volumes of seawater (1-100 ml), depending on cell concentration... -
Phytoplankton abundance and species composition in the North Balearic Sea in ...
Samples were collected with use of Niskin bottles and immediately fixed with formaldehyde (0.8% final concentration) for species identification and counts. -
Phytoplankton abundance and species composition in the Sicily Channel in Octo...
Samples were collected with use of Niskin bottles and immediately fixed with formaldehyde (0.8-1.6% final concentration) for species identification and counts. -
Epipelagic coccolithophores in the global oceans
Presence = 1, absence = 0. -
Range table from nannofossils in ODP Hole 195-1202B
This dataset has no description
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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... -
(Appendix C) Average nannofossil abundances in mid-Pliocene sediments from th...
This dataset has no description
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Coccolith percentage exclusive Emiliania huxleyi of surface sediment samples
This dataset has no description
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Nannofossil assemblage in surface sediments
This dataset has no description
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Distribution of nanoplankton at trap WR2
This dataset has no description
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(Table 6) Distribution of calcareous nannofossils in DSDP Hole96-624
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 5) Distribution of calcareous nannofossils in DSDP Hole 96-623
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 2) Distribution of calcareous nannofossils in DSDP Hole 96-622
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1... -
(Table 1) Distribution of calcareous nannofossils in DSDP Hole 96-621
Sediment depth is given in mbsf. Abundances: V = very abundant (10-100 specimens/field), A = abundant (1-10 specemens/field), C = common (1 specimen/2-10 fields), F = few (1...