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Range table from diatoms in ODP Hole 188-1167A
This dataset has no description
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Range table from diatoms in ODP Hole 188-1166A
This dataset has no description
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Range table from diatoms in ODP Hole 188-1165B
This dataset has no description
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Range table from diatoms in ODP Hole 188-1165A
This dataset has no description
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Diatom species of sediment core KNR197-10CDH42
This dataset has no description
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Diatom assemblages excluding Chaetoceros resting spores of sediment core JPC4...
Diatom abundance and assemblage data are presented for JPC43 - a ~12 m marine sediment core recovered from 576 m water depth in Neny Fjord, Marguerite Bay, Antarctic Peninsula... -
(Figure 4) Diatom species contribution in sediment core OCE326-GGC14
This dataset has no description
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(Table V) Distribution of diatoms in samples from Heidemann Valley trench, An...
Abundance estimates as follows: - = no specimens or fragments observed, 1 = at least one specimen or fragment per slide, R = a few specimens or fragments per slide, F = numerous... -
(Table 2b) Relative abundance of diatoms (Chaetoceros spp. resting spore-free...
Slides were prepared in a beaker with a diameter of 10 cm and the area of the microscope field of view used during counting was 0.000356 cm. The Hyalochaete Chaetoceros spp.... -
(Table T3) Diatom abundance in ODP Hole 188-1166A sediments
Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, Tr = trace, - = not found. -
(Table T2) Diatom abundance in ODP Hole 188-1165B sediments
Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, Tr = trace, - = not found. Abundance letter followed by 'r' = out of... -
Quarternary diatom abundance of sediment core CRP-1 (Table 2)
Numbers represent occurence in a count of 300 valves. <1 = whole specimens observed in sample but not recorded in initial count of 300 valves. <0.1 = identifiable... -
Diatom percentage abundances for sediment core KH-10-7 COR1GC from the Conrad...
Centennial and millennial scale variability of Southern Ocean temperature is poorly known, due to both short instrumental records and sparsely distributed high-resolution... -
(Table S1) Diatom abundance according to ice cycles in ANDRILL AND1-1B drill ...
The influence of Antarctica and the Southern Ocean on Late Pliocene global climate reconstructions has remained ambiguous due to a lack of well-dated Antarctic-proximal,... -
Diatom counts of Multicore OCE26MC25B
status of publication see PDI-148
