32 datasets found

We measured stable isotope and Mg/Ca ratio of planktonic foraminifera species Globorotalia tumida and Globorotalia crassaformis from IODP Site 363-U1489. Stable isotope...

Scyphozoan jellyfish in Icelandic waters have received limited attention, despite apparent recent increases in jellyfish blooms and considerable regional oceanographic and...

This dataset was obtained through field sampling conducted at two key research stations: the Ansai Comprehensive Soil and Water Conservation Experimental Station (Chinese...

Soil hydraulic parameters are vital for precise characterization of soil hydrological processes. Although many studies have integrated comprehensive soil datasets, availability...

Rewetting peatlands is an important measure to reduce greenhouse gas (GHG) emissions. However, after rewetting, the areas are highly heterogeneous in terms of GHG exchange,...

The values of δ18О in the ice wedges of northern Chukotka and paleotemperature characteristics during the Late Pleistocene and Holocene. Winter mean (twint.mean) and January...

Coastal ecosystems are heterogeneous environments with high turnover rates of carbon and nutrients that influence the distribution of greenhouse gases (GHG). They also represent...

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.

Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma.