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Seawater carbonate chemistry and variation in community development
Ocean acidification represents a pervasive environmental change that is predicted to affect a wide range of species, yet our understanding of the emergent ecosystem impacts is... -
Diverse coral communities in naturally acidified waters of a Western Pacific ...
Anthropogenic carbon dioxide emissions are acidifying the oceans, reducing the concentration of carbonate ions ([CO32-) that calcifying organisms need to build and cement coral... -
Physiological and ecological variables measured at the high and low pCO2 reef...
Experiments have shown that ocean acidification due to rising atmospheric carbon dioxide concentrations has deleterious effects on the performance of many marine organisms.... -
Paleoenvironmental indices across the PETM at El Dababiya GSSP, Egypt
This dataset has no description
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Benthic foraminiferal numbers of ODP Hole 171-1053B
This dataset contains the quantitative data relative to the benthic foraminifera assemblages from a subset of 26 samples from ODP Site 1053 core 8, Section 5. Samples span 74.54... -
Diatom composition of the sediment core EN18224-4 from Lake Satagay, Central ...
This dataset contains microscopic diatom counts from the sediment core EN18224-4, retrieved from Lake Satagay in Nyurbinsky District, Central Yakutia. The results include counts... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1052E (Table S3)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1050C (TAble S2)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1049C (Table S1)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Pollen taxa richness of sediment core PI-6 (85 ka BP) from Lake Petén Itzá, G...
Ostracodes and pollen preserved in a 75.9-m-long sediment core (PI-6) recovered from Lake Petén Itzá, Guatemala were used to assess the magnitude and velocity of aquatic and... -
Freshwater juvenile ostracode data of sediment core PI-6 (85 ka BP) from Lake...
Ostracodes and pollen preserved in a 75.9-m-long sediment core (PI-6) recovered from Lake Petén Itzá, Guatemala were used to assess the magnitude and velocity of aquatic and... -
Freshwater adult ostracode data of sediment core PI-6 (85 ka BP) from Lake Pe...
Ostracodes and pollen preserved in a 75.9-m-long sediment core (PI-6) recovered from Lake Petén Itzá, Guatemala were used to assess the magnitude and velocity of aquatic and... -
Benthic microalgal initial composition (relative abundances) and diversity in...
Relative abundance of benthic microalgae species was calculated based on total biomass in each initial community (A, B, and C). Species diversity measures are based on biomass... -
Benthic foraminiferal dynamics at Bottsand coastal lagoon (western Baltic Sea)
This dataset has no description
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Palynology of IODP Site 183-1138
This dataset has no description
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Counts of ostracode taxa from the Maastrichtian-Thanetian samples at IODP Sit...
This dataset has no description
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(Table 2) Assemblage densities and diversity of benthic foraminifera from dif...
This dataset has no description
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(Table 20) Ranges of benthic foraminifers from the late Neogene through the P...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 19) Ranges of benthic foraminifers from the late Neogene through the P...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because... -
(Table 18) Ranges of benthic foraminifers through the Neogene in DSDP Hole 23...
Benthic foraminifers were counted according to the following scheme: 1 = present, 2 = 2 or more, 3 = 3-5, 4 = 5-10, 6 = 10-30, 7 = 30-50, 8 = 50-75, and 9 = 75-150. Because...
