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(Figure 7) Sr/Ca and stable isotope anomalies across the thecal wall of three...
This dataset has no description
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(Figure 6) Sr/Ca and stable isotope records across a single thecal wall of co...
Distance=Y position -
(Figure 4 and Figure 5) 10-year long Sr/Ca and stable isotope records from in...
This dataset has no description
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Stable carbon and oxygen isotopes of benthic Uvigerina spp. in core M78/1_181-3
The Mississippi River discharge effectively shaped the dynamics of the Loop Current in the Gulf of Mexico during transient climates and interglacials, and reacted in response to... -
Stable carbon and oxygen isotopes and element ratios of planktic foraminifer ...
The Mississippi River discharge effectively shaped the dynamics of the Loop Current in the Gulf of Mexico during transient climates and interglacials, and reacted in response to... -
Monthly Bonaire coral Sr/Ca and oxygen isotope data from 118 kyr ago (coral B...
The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice... -
Raw data from 3.79 ka Bonaire coral, sample BON-7-A
Fossil coral / Age: 3793 +/- 29 yr BP, TIMS U-series date / Time period: 39 years around 3793 yr BP / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 2009 AD Bonaire coral, sample BON-0-A
Living modern coral / Top: January 2009 AD / Time period: 15 years before 2009 AD / Internal chronology starts at base (oldest part) of coral / Data acquired through subproject... -
Raw data from 1957 AD Bonaire coral, sample BON-9-B
Dead modern coral / Age: 1957 +/- 5 AD, TIMS U-series date / Time period: 13 years around 1957 AD / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 1912 AD Bonaire coral, sample BON-9-A
Dead modern coral / Age: 1912 +/- 8 AD, TIMS U-series date / Time period: 31 years around 1912 AD / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 6.22 ka Bonaire coral, sample BON-3-E
Fossil coral / Age: 6218 +/- 46 yr BP, TIMS U-series date / Time period: 67 years around 6218 yr BP / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 4.27 ka Bonaire coral, sample BON-4-G
Fossil coral / Age: 4268 +/- 25 yr BP, TIMS U-series date / Time period: 23 years around 4268 yr BP / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 3.83 ka Bonaire coral, sample BON-7-B
Fossil coral / Age: 3831 +/- 34 yr BP, TIMS U-series date / Time period: 33 years around 3831 yr BP / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 2.35 ka Bonaire coral, sample BON-6-A
Fossil coral / Age: 2347 +/- 49 yr BP, TIMS U-series date / Time period: 68 years around 2347 yr BP / Internal chronology starts at base (oldest part) of coral / Data acquired... -
Raw data from 1.84 ka Bonaire coral, sample BON-20-A
Fossil / Age: 1837 +/- 18 yr BP, TIMS U-series date / Time period: 7 years around 1957 AD / Internal chronology starts at base (oldest part) of coral / Data acquired through... -
(Fig. 4) Multiproxy data set of box core MSM5/5-712-1
A multiproxy data set of an AMS radiocarbon dated 46 cm long sediment core from the continental margin off western Svalbard reveals multidecadal climatic variability during the... -
Distribution of planktic foraminifera and stable istopes of sediment core MSM...
This dataset has no description
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40-year long monthly-resolved Sr/Ca record from 2.35 ka Bonaire coral, sample...
We present a 40-year long monthly resolved Sr/Ca record from a fossil Diploria strigosa coral from Bonaire (Southern Caribbean Sea) dated with U/Th at 2.35 ka before present... -
Results of the pollen analysis of the Dyanushka peat sediments K7/P2
A 415cm thick permafrost peat section from the Verkhoyansk Mountains was radiocarbon-dated and studied using palaeobotanical and sedimentological approaches. Accumulation of... -
Sea surface temperatures during Marine Isotope Stage (MIS) 11
The Marine Isotope Stage (MIS) 11 (424-374 ka) was characterized by a protracted deglaciation and an unusually long climatic optimum. It remains unclear to what degree the...
