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Iron physiology and metabolism of model phytoplankton taxa in the South Atlan...
Two diatoms (Cylindrotheca closterium) and two coccolithophores (Gephyrocapsa oceanica and Gephyrocapsa huxleyi, formerly Emiliania huxleyi) were isolated from inner and out... -
Seawater carbonate chemistry and polyphenols and carbohydrates of Emiliania h...
Cultures of the coccolithophore Emiliania huxleyi were grown under four different CO2-controlled pH conditions (7.75, 7.90, 8.10, and 8.25) to explore variations in extra- and... -
Multiple omics reveals coral reefs are living stones
Coral reefs are the cornerstone of global marine ecosystems, providing a shelter for over one third of marine organisms. In this bioproject, we have sequenced the genomes,... -
Dnmt1-Independent CG Methylation Contributes to Nucleosome Positioning in Div...
Dnmt1 epigenetically propagates symmetrical CG methylation in many eukaryotes. Their genomes are typically depleted of CG dinucleotides because of imperfect repair of deaminated... -
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... -
Collection of Marine Eukaryotes Transcriptomes
This project is part of the Marine Eukaryotes Transcriptomes initiative providing a comprehensive resource of marine eukaryotes plankton transcriptomes homogeneously assembled... -
(Table T2) Occurrence of calcareous nannofossils with zonal assignments, ODP ...
Table note: + = present, - = not present -
(Table T2) Occurrence of calcareous nannofossils with zonal assignments, ODP ...
Table note: + = present, - = not present -
(Table T2) Distribution of Pleistocene calcareous nannofossils, ODP Hole 178-...
Table notes: * = very dissolved and overgrown. Abundance: A = abundant, C = common, F = few, R = rare, X = scarce, B = barren. Preservation: P = poor, M = moderate. -
(Table T3) Distribution of Pleistocene calcareous nannofossils, ODP Hole 178-...
Table notes: Abundance: A = abundant, C = common, F = few, R = rare, X = scarce, B = barren. Preservation: P = poor, M = moderate. -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) - Wadden Se...
In order to monitor long-term variability in or eventual change of the planktonic community a semiquantitative analysis of microplankton based on net sampling is ongoing since... -
Semi-quantitative microplankton analysis (Sylt Roads Time Series) - Wadden Se...
In order to monitor long-term variability in or eventual change of the planktonic community a semiquantitative analysis of microplankton based on net sampling is ongoing since... -
Seawater carbonate chemistry, nutrients, particulate carbon and growth rate o...
The response of Emiliania huxleyi (Lohmann) W. W. Hay et H. Mohler, Calcidiscus leptoporus (G. Murray et V. H. Blackman) J. Schiller, andSyracosphaera pulchra Lohmann to... -
Seawater carbonate chemistry and processes during experiments with Emiliania ...
Ocean acidification in response to rising atmospheric CO2 partial pressures is widely expected to reduce calcification by marine organisms. From the mid-Mesozoic,... -
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
