Sediment components of core L009/21@en

DataONE2026-02-15 更新2026-05-19 收录

碳十四测年校正

海洋储库效应

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Ages corrected for an ocean reservoir age of 400 14C yr

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2026-05-01

(Table S1) 14C-AMS dates used for the chronology of sediment core GeoB9307-3

沉积物年代学

碳十四测年校正

Conversion of radiocarbon ages to calendar ages was done using the program Calib 6.0.1**25 and the Marine09 calibration curve**26. A regional reservoir age offset of +140±25 years was applied**27. Age

DataONE2025-01-10 更新40

(Table 3) Calculation of the local marine reservoir effect based on six paire...

放射性碳定年校正

海洋储库效应

Calculation of the local marine reservoir effect (DeltaR = -25 ± 45 years).Marine model 14C age was reversely calculated using the method of Yu et al. (2010) so that the...

B2FIND20

(Table 1) Radiocarbon ages and carbon isotopic values of Portlandia shells in sediment cores BP00-07/06 and BP00-23/07

碳十四测年校正

水库年龄校正

For all further calculations given in the article, the ages were corrected for the reservoir age of 440 yr and transformed into the calendar age.

PANGAEA2004-01-01 更新00

(Table 2) Radiometric data of sediment core PG1901, Lake Donggi Cona@en

沉积物年代学

碳十四测年校正

Corrected ages adjusted using the lake reservoir effect determined for a core-top sample. Calibrated ages were calculated with OxCal 4.1 and the IntCal09 calibration curve (Bonk Ramsey, 2009; Reimer e

DataONE2026-02-15 更新20

Marine radiocarbon reservoir ages for the past 50,000 years, links to model r...

放射性碳测年校准

海洋储库效应

Radiocarbon (14C) dating calibration for the last glacial period largely relies on cross-dated marine 14C records. However, marine reservoirs are isotopically depleted with...

B2FIND00

Sediment components of core L009/21@en

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