K isotopes trace temporal silicate weathering intensity

Silicate weathering alters the biogeochemical compositions of the lithosphere, hydrosphere, and atmosphere, and thereby regulates both nutrient cycling and habitable temperatures on Earth, but tracing silicate weathering effectively remains a challenge. Potassium (K) isotopes have been proposed as a tracer of silicate weathering intensity spatially, but there is a significant gap in how and why K isotopes trace silicate weathering temporally. Here we investigate seasonal variations in dissolved K isotopes in the middle Yellow River, which drains a large area of homogeneous loess that represents the average geochemical composition of the upper continental crust, and experiences significant climatic seasonality driven by the East Asian monsoon. We find that K isotopes show strong seasonality as a function of aluminosilicate neoformation following silicate dissolution, and thus could serve as a tracer of silicate weathering intensity. We derive an empirical relationship of δ<sup>41</sup>K<sub>rw</sub> = -0.07 × ln(W/D) - 0.38, where W(silicate chemical weathering)/D(denudation) refers to silicate weathering intensity.

Authors

Institutions

Publication Details

Journal
Nature Communications
Published
2025-12-09
DOI
https://doi.org/10.1038/s41467-025-67085-w
Primary Topic
Silicon Effects in Agriculture
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

K isotopes trace temporal silicate weathering intensity

Zhi‐Qi Zhao, Hai‐Ou Gu, David J. Wilson, W. Li et al.
Nature Communications
Silicon Effects in Agriculture
article

K isotopes trace temporal silicate weathering intensity

Zhi‐Qi Zhao, Hai‐Ou Gu, David J. Wilson, W. Li, Αlbert Galy, Philip A.E. Pogge von Strandmann, Jun Xiao, He Sun, Zhangdong Jin, Long‐Fei Gou
article en

Abstract

Silicate weathering alters the biogeochemical compositions of the lithosphere, hydrosphere, and atmosphere, and thereby regulates both nutrient cycling and habitable temperatures on Earth, but tracing silicate weathering effectively remains a challenge. Potassium (K) isotopes have been proposed as a tracer of silicate weathering intensity spatially, but there is a significant gap in how and why K isotopes trace silicate weathering temporally. Here we investigate seasonal variations in dissolved K isotopes in the middle Yellow River, which drains a large area of homogeneous loess that represents the average geochemical composition of the upper continental crust, and experiences significant climatic seasonality driven by the East Asian monsoon. We find that K isotopes show strong seasonality as a function of aluminosilicate neoformation following silicate dissolution, and thus could serve as a tracer of silicate weathering intensity. We derive an empirical relationship of δ<sup>41</sup>K<sub>rw</sub> = -0.07 × ln(W/D) - 0.38, where W(silicate chemical weathering)/D(denudation) refers to silicate weathering intensity.

Nature CommunicationsVol. 17(1)
Centre National de la Recherche Scientifique (FR), Hefei University of Technology (CN), Johannes Gutenberg University Mainz (DE), Chang'an University (CN), China University of Geosciences (CN), Centre de Recherches Pétrographiques et Géochimiques (FR), Institute of Earth Environment (CN), University College London (GB)
National Natural Science Foundation of China, Hefei University, Hefei University of Technology, Natural Environment Research Council
Openalex Percentile: Top 71%
Silicon Effects in Agriculture
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.