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Seawater carbonate chemistry and particulate inorganic carbon, particulate or...
Coccolithophores are unicellular marine phytoplankton and important contributors to global carbon cycling. Most work on coccolithophore sensitivity to climate change has been on... -
(Table 11) Distribution of Pleistocene to early Pliocene nannofossils in ODP ...
Species abundance: A = abundant (>10% of the total assemblage), C = common (1.0-10%), F = few (0.1-1.0%), R = rare (<0.1%), r = reworked, - = absent. -
(Table 7) Distribution of Pleistocene to Miocene nannofossils in ODP Hole 108...
Species abundance: A = abundant (>10% of the total assemblage), C = common (1.0-10%), F = few (0.1-1.0%), R = rare (<0.1%), r = reworked, - = absent. -
(Appendix C) Average nannofossil abundances in mid-Pliocene sediments from th...
This dataset has no description
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Nannofossil abundance of Hole 47-397
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 47-397
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Global SEM coccolithophore abundance compilation
Coccolithophores are globally important marine calcifying phytoplankton. They contribute to the organic carbon pump through the primary production and the ballast of organic... -
Epipelagic coccolithophores in the global oceans
Presence = 1, absence = 0. -
Fossil occurrence of calcareous nannofossils from IODP Hole 315-C0002D
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Fossil occurrence of calcareous nannofossils from IODP Hole 315-C0002B
Geocode = [m CSF-A] Top Core depth (below sea floor) -
Marine Microbial Eukaryote Transcriptome Sequencing Project
The Marine Microbial Eukaryote Transcriptome Sequencing Project was a collaboration between the National Center for Genome Resources, the Gordon and Betty Moore Foundation's... -
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 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... -
Living coccolithophore abundance from the Ebro Delta coastal area during MERS...
The present dataset contains coccolithophores abundances (coccospheres/L). The samples were collected between Barcelona and the Ebro Delta (Western Mediterranean), during the... -
Benthic foraminifera and nannofossil abundance of Hole 40-364
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Benthic foraminifera and nannofossil abundance of Hole 40-360
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
