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(Table T1) Neogene stratigraphy of diatoms, ebridians and endoskeletal dinofl...
Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, X = present, B = barren, r = rare occurrences of a taxon interpreted... -
(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... -
Diatom assamblage in samples from sediment trap NBP96-04A_MS7a_trap
Numbers represent the calculated diatom flux as recorded by the mooring, and the individual species counts. The diatom flux [#/m**2/day] was calculated using two different... -
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... -
Coccolithophore and diatom cell abundance from the upper mixed later of the G...
This data was collected as part of the Great Calcite Belt project, from 60W to 120E and 30S to 60S. during MV1101 onboard R/V Melville, January- February 2011 in the South... -
(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,...