The silicate weathering of continental rocks plays a vital role in determining ocean chemistry and global climate. Spatiotemporal variations in the Li isotope ratio (δ7Li) of terrestrial waters can be

NIAID Data Ecosystem10

Data for: Early Cretaceous mafic-intermediate dykes in the Dabie orogen as indicators for post-collisional lithosphere removal

岩石圈减薄

同位素地球化学

Table S1 U-Pb O isotopes of xenocrystic zircons from mafic-intermediate dykes in Dabie orogen

Mendeley Data00

(Appendix B2) Stable carbon and oxygen isotope ratios of the fine fraction se...

同位素地球化学

沉积学

Sediment depth is given in mbsf, fine fraction <10 µm. For isotope data of Bohaty and Zachos (2003) see dataset: doi:10.1594/PANGAEA.713537.

B2FIND20

Authigenic neodymium isotope data from ODP site 108-659 since the last glacial

古海洋学

同位素地球化学

Authigenic Fe-Mn oxyhydroxide derived neodymium isotope data since the last glacial extracted by weekly reductive leaching. Isotope ratios are normalized to 146Nd/144Nd = 0.7219 and were analyzed on t

PANGAEA2020-01-01 更新00

Data for: Potassium isotope systematics of oceanic basalts

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