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(Table 1) Planktonic foraminifera community at DSDP Hole 94-608
VR = very rare, R = rare, C = common, A = abundant, X = reworked, cf. = compare, - = absent. -
(Table 5) Eocene to Oligocene nannofossil range chart for ODP Hole 134-829A
Species abundance: H = highly abundant: 101-1000 specimens per field of view; V = very abundant: 11-100 specimens per field of view; A = abundant: 1-10 specimens per field of... -
(Table 5) Oligocene to Pleistocene nannofossil range chart for ODP Hole 134-829A
Species abundance: H = highly abundant: 101-1000 specimens per field of view; V = very abundant: 11-100 specimens per field of view; A = abundant: 1-10 specimens per field of... -
(Table 19) Nannoplankton distribution in sediment core ANS3-T9
Species abundaces: C = common, F = few, R = rare, VR = very rare, - = absent. -
(Table 18) Nannoplankton distribution in sediment core ANS3-T6
Species abundaces: C = common, F = few, R = rare, VR = very rare, - = absent. -
(Table 17) Nannoplankton distribution in sediment core ANS3-T4
Species abundaces: C = common, F = few, R = rare, VR = very rare, - = absent. -
(Table 16) Nannoplankton distribution in sediment core ANS3-T1
Species abundaces: C = common, F = few, R = rare, VR = very rare, - = absent. -
(Table T1) Census counts of radiolarian taxa in ODP Hole 175-1082A
Abundance: A = abundant; >10,000 specimens on a slide. C = common; 1001-10,000 specimens on a slide. F = few; 501-1000 specimens on a slide. R = rare; 11-500 specimens on a... -
Chlorophyll a, extracellular polymeric substance concentration and 16S rRNA g...
Samples were taken to study the effect of storm surges on ecosystem functioning of salt marsh microbial communities. Sediment samples were collected from experimental salt marsh... -
Abundance of larvae and transforming stages of mesopelagic fish collected at ...
This file contains data on numerical abundance of larvae and transforming stages of fishes collected during the CSIC-SUMMER survey carried out in October 2010 in five zones... -
Seawater carbonate chemistry and calcification rate of reef-building coral Si...
Anthropogenic increases in atmospheric CO2 over this century are predicted to cause global average surface ocean pH to decline by 0.1–0.3 pH units and sea surface temperature to... -
Seawater carbonate chemistry and physiological parameters of Caribbean coral
Global change driven by anthropogenic carbon emissions is altering ecosystems at unprecedented rates, especially coral reefs, whose symbiosis with algal symbionts is... -
Southern Ocean RADiolarian dataset (SO-RAD)
Radiolarians (holoplanktonic Protozoa) found in marine sediments are commonly used in Southern Ocean as palaeoclimate proxies. Generating such reconstructions of past climate... -
Occurrence and cover of algae along a transect at the island of Helgoland in ...
A sublittoral transect (P3) in the North of Helgoland that had been investigated ~40 years earlier by Lüning (1970) was traversed again. Scuba dives were carried out between... -
Harmonized in-situ observations of surface energy fluxes and environmental dr...
Despite the importance of surface energy budgets (SEBs) for land-climate interactions in the Arctic, uncertainties in their prediction persist. In situ observational data of SEB... -
Carbon stocks and carbon accumulation rates of sediment cores in Clayoquot So...
The goal of this project was to provide the first estimates of blue carbon stocks and carbon accumulation rates in the high and low marsh zones of salt marshes from the Pacific... -
Morphotype counts of Emiliania huxleyi coccoliths from surface sediment sampl...
This dataset has no description
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Microhabitat distribution in sympatric populations of closely related species...
This dataset contains microhabitat distribution data. -
Pollen counts from short monoliths (FRK III and FRK IV) blanket bog at Connem...
Analyst: Michael O'ConnellLaboratory: Palaeoenvironmental Research Unit, NUI Galway, Galway, IrelandData analysis completed: 1987Sampling in field: 1985-08-20. Sample density:...
