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Palynologycal record of a long sediment core from Lake Shira (Minusinsk Depre...
In 2022, a 530 cm long sediment core (Shira core 3, 54°31̍18,2̎ N, 90°10̍43,7̎ E) was recovered from 24 m depth in the central part of Lake Shira. Lake Shira is located in... -
Dead Sea lake level for the last 237 ka, 95% CI calculation
This dataset has no description
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Dead Sea lake level for the last 237 ka, data compilation
This dataset has no description
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South Pacific Convergence Zone (SPCZ) sediment core age models
Age model dates is SPCZ 14C and 210Pb dates used for BACON age models from Lac Lanutavake (cores UC1 and UC4 combined for a single age model), Lac Lalolalo (cores UC13, UC14,... -
South Pacific Convergence Zone (SPCZ) Titanium data
SPCZ Titanium data from Lake Lanoto'o on 'Upolu (Samoa), and Lake Emaotul on Efate (Vanuatu) -
South Pacific Convergence Zone (SPCZ) magnetic susceptibility
South Pacific Convergence Zone (SPCZ) d2Hdinosterol and calculated precipitation values (where SPCZ magnetic susceptibility (where available) from Lac Lanutavake (duplicate... -
South Pacific Convergence Zone (SPCZ) d2Hdinosterol and calculated precipitat...
South Pacific Convergence Zone (SPCZ) d2Hdinosterol and calculated precipitation values (where appropriate) from Lac Lanutavake (duplicate cores UC1 and UC4), Lac Lalolalo... -
Contrasting Common Era climate and hydrology sensitivities from paired lake s...
Hydroclimate on 'Uvea (Wallis et Futuna) is controlled by rainfall associated with the South Pacific Convergence Zone (SPCZ), the southern hemisphere's largest precipitation... -
Trace elements in ostracod valves of TAN12-2 from Tangra Yumco (Table 2)
This dataset has no description
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Trace elements in ostracod valves of NC08/01 from Nam Co (Table 1)
This dataset has no description
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Stable isotopes in bulk sediment TAN12-2 (Table 4)
This dataset has no description
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Stable isotopes in ostracod shells of core NC08/01 (Table 3)
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Pollen and spore record of lake sediments, the southern part of the Yamal pen...
Palynological data have been obtained from the lake sediments, the southern part of the Yamal peninsula. For the spore-pollen analysis we used a 30 cm core of bottom sediments... -
Trace elements, stable isotopes and rare earth elements in ostracod valves fr...
High-resolution multi-proxy records from two lakes on the southern Tibetan Plateau, Nam Co and Tangra Yumco, are used to infer long-term variations in the Asian monsoon system.... -
Diatom-bound and bulk sediment nitrogen isotope ratios, bulk sediment paramet...
In two corresponding sediment cores (Figino19-2 and Figino18-2) from the South Basin of Lake Lugano (Switzerland), we have measured diatom-bound nitrogen isotopes, bulk sediment... -
Dead Sea lake level for the last 237 ka reconstructed with deep core halite f...
The rain regime in the Eastern Mediterranean is primarily controlled by Mediterranean winter cyclonic systems. The lake level of the Dead Sea responds sensitively to... -
XRF, grain size, and biogeochemical characteristics of a sediment core from L...
Eight overlapping sediment cores, representing an approximately 6.6 m–long composite sequence, were collected on March 24, 2013 from Lake Malaya Chabyda in Central Yakutia... -
River connectivity and climate behind the long-term evolution of Tropical Ame...
This study presents the long-term evolution of two floodplains lakes (San Juana and Barbacoas) of the Magdalena River in Colombia with varying degree of connectivity to the... -
Geochemical sediment core data (KK 12-1 and KK 12-2) covering 31 kyrs from La...
The Central Asian Pamir Mountains (Pamirs) are a high-altitude region sensitive to climatic change, with only few paleoclimatic records available. To examine... -
Sedimentation rate of sediment cores Figino19-2 from lake Lugano, Switzerland
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