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(Table S1) Boron isotope and trace element data and reconstructed carbonate s...
The middle Miocene Climatic Optimum (17-15 Ma; MCO) is a period of global warmth and relatively high CO2 and is thought to be associated with a significant retreat of the... -
Experiment treatments for sea urchin larvae in response to Vibrio infection u...
This dataset has no description
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Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Measurements of microbial processes, dissolution, water and porewater chemist...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
Chironomid determination of sediment core from Lake Prata (São Miguel, Azores...
The location of the Azores Archipelago makes this group of islands an excellent setting for investigating past long-term temperature and precipitation changes in the central... -
(Table 5) Results obtained on width of roots from the Post-hoc multiple compa...
This dataset has no description
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(Table 4) Results obtained on length of roots from the Post-hoc multiple comp...
This dataset has no description
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(Table 3) Results obtained on number of roots from the Post-hoc multiple comp...
This dataset has no description
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Database of metal concentrations measured in sediment cores (1965-2011) and b...
This database contains metal element concentrations from (1) river sediment cores and (2) bed and flood deposits acquired along the Rhône River by research teams (for 1:... -
Neodymium isotopes, planktic and benthic stable carbon and oxygen isotopes, s...
Neodymium isotope data measured on mixed species of uncleaned planktic foraminifera, planktic (G. bulloides) and benthic (C. kullenbergi) stable carbon and oxygen isotopes, mean... -
(Table S5) Regional stacks of SST estimates as a function of age, Region 4 NH...
This sheet differs from the original version published as Herbert et al. (2016). The age models for Sites 151-907 and 162-982 were updated in October 2017, resulting in... -
(Table AT9) Palaeomagnetic analysis of ODP Hole 207-1260B
Sediment depth is given in mcd. -
(Table AT8) Palaeomagnetic analysis of ODP Hole 207-1260A
Sediment depth is given in mcd. Between 25R-1,12 and 25R-3,91: Biostrat gap of P9 = C22n and C22r = between 24R-CC and 25R-1, 50 cm; but uncertain about the above sample. -
(Table AT7) Palaeomagnetic analysis of ODP Hole 207-1259B
Sediment depth is given in mcd. Between 2R-7,7 and 4R-1,64: Gap = C23r? But minor in MCD? -
(Table AT6) Palaeomagnetic analysis of ODP Hole 207-1259A
Sediment depth is given in mcd. Between 32R-2,29 and 34R-1,31: GAP, maybe C22r? -
(Table AT5) Palaeomagnetic analysis of ODP Hole 207-1258B
Sediment depth is given in mcd. -
(Table AT4) Palaeomagnetic analysis of ODP Hole 207-1258A
Sediment depth is given in mcd. -
(Table AT3) Maastrichtian-Campanian palaeomagnetic analysis of ODP Hole 207-1...
Sediment depth is given in mcd. -
(Table AT2) Late Eocene-Albian palaeomagnetic analysis of ODP Hole 207-1257B
Sediment depth is given in mcd. Additional comments: Between 1R-2,47 and 1R-3,48: Possible gap of P15 foram zone (uppermost middle Eocene; lower upper Eocene); between 3R-4,36... -
(Table AT1) Early Maastrichtian to mid-Campanian palaeomagnetic analysis of O...
Sediment depth is given in mcd.
