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Deep-sea megabenthic fauna type from ROV transects of MEDWAVES survey
Dataset encompasses identification and quantitative information on megabenthic fauna and substrate characterization resulted from the processing of ROV video transects acquired... -
Larval release rate of the scleractinian cold-water coral Caryophyllia huinay...
To describe the metamorphosis and post-larval development stages of the scleractinian cold-water coral Caryophyllia huinayensis adults were collected at Comau Fjord, Chile, and... -
Seawater carbonate chemistry and kelp densities and coral coverages at three ...
Ocean warming is altering the biogeographical distribution of marine organisms. In the tropics, rising sea surface temperatures are restructuring coral reef communities with... -
(Appendix 1) Coral analysis and isostatic rebound effects from different Hole...
Past sea-level records provide invaluable information about the response of ice sheets to climate forcing. Some such records suggest that the last deglaciation was punctuated by... -
Percentage cover of coral, sponges, substrates with environmental variables a...
This dataset has no description
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(Table 5) Distribution of foraminifera in the Miocene section of ODP Hole 133...
X = present, - = absent, ? = questionable occurrence -
(Table 4) Distribution of foraminifera in the Miocene section of ODP Hole 133...
X = present, - = absent, ? = questionable occurrence -
(Table 3) Distribution of foraminifera in the Miocene section of ODP Hole 133...
X = present, - = absent, ? = questionable occurrence -
(Table 2) Distribution of foraminifera in the Miocene section of ODP Hole 133...
X = present, - = absent, ? = questionable occurrence -
(Table 2) Distribution of early late Eocene fossil content in ODP Hole 115-714A
Abundances: A = abundant, C = common, P = present. -
(Table 1) Distribution of early late Eocene fossil content in ODP Hole 115-715A
Abundances: A = abundant, C = common, P = present. -
(Table S1) Uranium and Thorium isotopes and U/Th ages of IODP Exp310 cores fr...
The timing of sea-level change provides important constraints on the mechanisms driving Earth's climate between glacial and interglacial states. Fossil corals constrain the... -
Texture description and distribution of components in ODP Hole 103-639D (Figu...
A detailed analysis of the texture, matrix, and elements of the microfacies from the carbonate sequence recovered in ODP Hole 639D resulted in a typological classification of 10... -
Vertical distribution of macrofossil taxa in ODP Hole 122-764B
Rhaetian fossil reef was penetrated on the Wombat Plateau (northern Exmouth Plateau, northwest Australia). A study of fossil populations and associated sediment types showed a... -
Coral-based composite indices of sea surface temperature and salinity variabi...
Coral-based proxy records from four long lived Porites sp. cores along the South Pacific Convergence Zone maximum precipitation diagonal axis (RO2 - Rotuma, 1F - Fiji, TNI2 -... -
Global marine radiocarbon data compilation for the last deglaciation, spline ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, global ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, zonal a...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Effects of elevated pCO2 and feeding on net calcification and energy budget o...
Ocean acidification is a major threat to calcifying marine organisms such as deep-sea cold-water corals (CWC), but related knowledge is scarce. The aragonite saturation...
