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(Table T7) Coarse-fraction particle counts, ages, and linear sedimentation ra...
This dataset has no description
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(Table T7) Coarse-fraction particle counts, ages, and linear sedimentation ra...
This dataset has no description
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(Appendix A) Coarse-Fraction Values, Hole 178-1095B
This dataset has no description
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(Table T7) Diatom percentages of ODP Site 178-1101
This dataset has no description
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(Table T4) Diatom percentages of ODP Hole 178-1096B
This dataset has no description
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(Table T4) Diatom percentages of ODP Hole 178-1096A
This dataset has no description
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(Table T1) Diatom percentages of ODP Site 178-1095
This dataset has no description
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(Table T2) Percentage and absolute abundance of major diatom species in ODP H...
Percentage of major diatom species, actual number of diatoms counted in each sample, and diatom abundance. -
(Table T3) Ratio of symmetric to asymmetric forms of Eucampia antarctica in O...
This dataset has no description
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(Table T2) Dinoflagellate cyst occurrence in neogene sediments of ODP Hole 17...
This dataset has no description
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(Table T2) Dinoflagellate cyst occurrence in neogene sediments of ODP Hole 17...
This dataset has no description
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(Table T2) Dinoflagellate cyst occurrence in neogene sediments of ODP Hole 17...
This dataset has no description
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Stable isotopes and mol% of amino acids in 0.2-3 µm seston at surface during ...
The Amazon river accounts annually for 20% of riverine discharge into the global ocean with strong seasonal variations. This lens of freshwater spreads at surface as a plume,... -
Stable isotopes and mol% of amino acids in 3-200 µm seston at surface during ...
The Amazon river accounts annually for 20% of riverine discharge into the global ocean with strong seasonal variations. This lens of freshwater spreads at surface as a plume,... -
Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment sig...
The Labrador Sea is an ideal region to study the biogeographical, physiological and biogeochemical implications of phytoplankton communities due to sharp transitions of distinct... -
Holocene δ¹⁸O diatom from ODP Hole 178-1098A
The causes for rising temperatures along the Antarctic Peninsula during the late Holocene have been debated, particularly in light of instrumental records of warming over the... -
Diatom isotope data from ODP Hole 178-1098A for the last deglaciation (12.2-1...
Understanding the response of the Antarctic ice sheets during the rapid climatic change that accompanied the last deglaciation has implications for establishing the... -
Hydrochemistry measured with a FerryBox system at time series station Helgola...
This dataset has no description
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Hydrochemistry measured with a FerryBox system at time series station Helgola...
This dataset has no description
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Hydrochemistry measured with a FerryBox system at time series station Helgola...
Depth in water = 1 indicates than depth is not given
