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(Appendix 3B) Varimax factor score matrix for benthic foraminifera in eastern...
This dataset has no description
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(Appendix 3A) Principal factor score matrix for benthic foraminifera in easte...
This dataset has no description
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Paleomagnetic of sediment core DVDP-11
This dataset has no description
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Paleomagnetic of sediment core DVDP-10
This dataset has no description
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Paleomagnetic of sediment core CIROS-2
This dataset has no description
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Stable isotope data and statistics of core M25/4-KL13
This dataset has no description
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(Table 4) Principal component analysis, paleotemperatures and distribution of...
This dataset has no description
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(Table 4) Principal component analysis, paleotemperatures and distribution of...
This dataset has no description
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(Table 4) Principal component analysis, paleotemperatures and distribution of...
This dataset has no description
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(Table 4) Principal component analysis, paleotemperatures and distribution of...
This dataset has no description
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(Appendix B) Benthic foraminiferal abundances and principal component scores ...
Age model of Baldauf et al. (1986) -
(Appendix A) Benthic foraminiferal abundances and principal component scores ...
Age model of Baldauf et al. (1986) -
(Appendix 5) Principal Component Scores of benthic foraminifera Q-mode assemb...
This dataset has no description
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XRF analysis of sediment core from Asea (Peloponnese, Greece) for the Late Ho...
The sediment core Asea-1 was retrieved from the Asea Valley, Peloponnese Greece, in 2010 using a vibra corer. The upper 5 m were scanned at 0.5 cm resolution with... -
Paleosecular geomagnetic variation for the Holocene measured from U-channels ...
Inclination, declination, and relative palaeointensity calculated as a composite (WINPSV-12K) of four sediment cores (+54-03/57PC, +54-03/64PC, +54-03/67PC, +54-03/68PC) from... -
A Late Pleistocene sea level stack
Late Pleistocene sea level has been reconstructed from ocean sediment core data using a wide variety of proxies and models. However, the accuracy of individual reconstructions... -
(Table S2) Biometric data, time of ice breakup and carbon isotopic compositio...
Two global environmental issues, climate change and contamination by persistent organic pollutants, represent major concerns for arctic ecosystems. Yet, it is unclear how these... -
(Table T1) Paleomagnetic properties of ODP Hole 191-1179D basalts
During Ocean Drilling Program Leg 191, ~100 m of mid-Cretaceous igneous crust was cored at Site 1179 (41.08°N, 159.96°E), located within magnetic Anomaly M8 on the abyssal plain... -
(Table T1) Paleomagnetic characterization of sedimentary rocks from ODP Hole ...
Coring in Hole 1213B on the south flank of Shatsky Rise recovered sedimentary rocks (chalk and claystone) of earliest Cretaceous (Berriasian) age. Because few samples of this...
