Dataset - B2FIND

Bottom water oxygen qualitative reconstruction for sediment core MD07-3100

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Bottom water oxygen qualitative reconstruction for sediment core MD07-3088

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Seasonal chamber measurements of CH4 fluxes and pore water data from vegetati...

The data set contains chamber measurements of methane (CH4) emissions from vegetation removal experiments consisting of three vegetation treatments (intact vegetation, vascular...

Seasonal chamber measurements of CH4 fluxes and their isotopic composition al...

The data set contains measurements of methane (CH4) emissions and their δ13C values at vegetation removal experiments consisting of three vegetation treatments (intact...

(Supplement Table 3) Mean annual precipitation reconstruction derived from th...

Mean annual precipitation reconstruction derived from the A/C ratio from the TMD composite core from Tso Moriri using the described exponential regression model (see Chapter...

Quantitative reconstruction of Holocene sea ice and sea surface temperature o...

Holocene oceanographic conditions in Disko Bay, West Greenland were reconstructed from high-resolution diatom records derived from two marine sediment cores. A modern dataset...

Record of oxygen and carbon stable isotopes and reconstructed oxygen concentr...

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Oxygen isotope (δ¹⁸O) values of benthic ostracods from varved sediments from ...

The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger...

Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926

Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of...

(Table S3) Percentage pollen diagram representing 38 fossil pollen spectra of...

Relative pollen percentages are calculated upon the sum of 32 tree and shrub pollen taxa taken as 100% following Gotanda et al. (2002). Reconstructed dominant biomes derived by...

Borneo stalagmite SC02 temperature reconstructions over Termination I by the ...

This dataset presents cave temperatures over the last glacial termination from stalagmite SC02 from Secret Cave in Mulu, Northern Borneo (4.063°N, 114.833°E). The temperatures...