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(Table 1) Microbialites from coral reefs off the volcanic islands Tahiti and ...
Contents of CaCO3, total organic carbon (TOC), total sulfur (TS, non-carbonate = decalcified rest of sample), and chromium reducible sulfur (CRS, representing sulfide minerals... -
(Supplement 1) All detected fatty acids and their compound-specific carbon is...
Sediment depth is given in mbsf. # = either trace amounts or not detected or not measureable, please have a look at the publication. * = minor co-elution with other minor... -
(Table 4) Fatty acids and alcohols analysis and their compound-specific carbo...
Sediment depth is given in mbsl. # = either trace amounts or not detected or not measureable, please have a look at the publication. -
(Supplement 3) Lipid- and group-specific proportions and their mean compound-...
Sediment depth is given in mbsf. Empty fields are either trace amounts or not detected or not measureable, please have a look at the publication.sat. = saturated. -
(Supplement 2) All detected alcohols and their compound-specific carbon isoto...
Sediment depth is given in mbsf.# = either trace amounts or not detected or not measureable, please have a look at the publication -
(Table 3) Analysis of non-carbonate fractions from different Holes of IODP Ex...
Sediment depth is given in mbsf.Empty fields = trace amounts -
(Table 2) Elemental contents expressed as ratios versus Ca from different Hol...
This dataset has no description
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(Table 1) Growth patterns of microbialites, water depths and applied methods ...
This dataset has no description
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(Table 3) Different age analysis from different Holes of IODP Expedition 310
(#) = Radiocarbon ages were calibrated using CALIB REV 5.0.1 Stuiver & Reimer (1993) and the marine 04.14 c dataset Hughen et al. (2004) with a further adjustment of a... -
(Table 2) Water depths and the stratigraphical position from different Holes ...
Sediment depth is given in mbsl. -
(Table 2) Age calculation and calcite concentration from IODP Hole 310-M0005D
Sediment depth is given in mbsl. # = data have been previously published by Thomas et al. (2009) -
(Table 1) Uranium and thorium concentrations as well as isotope ratios from I...
This dataset has no description
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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... -
(Table 1) Different age analysis from IODP Site 310-M0018A
Deglacial reefs from Tahiti (IODP 310) feature a co-occurrence of zooxanthellate corals with microbialites that compose up to 80 vol% of the reef framework. The notion that... -
Nongeniculate coralline algae from IODP Site 310-M0005D
Material cored during the Integrated Ocean Drilling Program (IODP) Expedition 310 'Tahiti Sea Level' revealed that the fossil reef systems around Tahiti are composed of two... -
Isotope analysis, age calculation and calcite concentration from IODP Hole 31...
We present uranium-thoriumchronology for a 102 mcore through a Pleistocene reef at Tahiti (French Polynesia) sampled during IODP Expedition 310 "Tahiti Sea Level". We employ... -
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... -
(Table SD1, Fig. 2) Benthic foraminiferal abundances, preservation states and...
This dataset has no description
