- Research Briefing
- Published:
Drought-induced secondary carbonate formation restricts lateral carbon transport
Nature Geoscience (2025)Cite this article
-
128 Accesses
Subjects
Over a prolonged period of hydrologic drought, the major ion chemistry of a North American river dramatically shifted, revealing reduced lateral carbon transport due to secondary carbonate formation. These observations expose a natural limit to the inorganic carbon carrying capacity of rivers.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
9,800 Yen / 30 days
cancel any time
Subscription info for Japanese customers
We have a dedicated website for our Japanese customers. Please go to natureasia.com to subscribe to this journal.
Prices may be subject to local taxes which are calculated during checkout
References
Regnier, P. et al. Anthropogenic perturbation of the carbon fluxes from land to ocean. Nat. Geosci. 6, 597–607 (2013). This paper presents perturbations to carbon fluxes due to anthropogenic activity.
Raymond, P. A. & Hamilton, S. K. Anthropogenic influences on riverine fluxes of dissolved inorganic carbon to the oceans. Limnol. Oceanogr. Lett. 3, 143–155 (2018). This paper presents human influences on riverine DIC fluxes.
Beerling, D. J. et al. Enhanced weathering in the US Corn Belt delivers carbon removal with agronomic benefits. Proc. Natl Acad. Sci. USA 121, e2319436121 (2024). This paper presents EW as a carbon sequestration strategy.
Wang, J. et al. Sampling frequency, load estimation and the disproportionate effect of storms on solute mass flux in rivers. Sci. Total Environ. 906, 167379 (2024). This paper offers a more detailed description of our RiverLab.
Knapp, W. J. & Tipper, E. T. The efficacy of enhancing carbonate weathering for carbon dioxide sequestration. Front. Clim. https://doi.org/10.3389/fclim.2022.928215 (2022). This paper shows that many major rivers are poised at or above calcite saturation.
Additional information
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
This is a summary of: Wang, J. et al. Drought constrictions on lateral carbon transport. Nat. Geosci. https://doi.org/10.1038/s41561-025-01807-z (2025).
Rights and permissions
About this article
Cite this article
Drought-induced secondary carbonate formation restricts lateral carbon transport. Nat. Geosci. (2025). https://doi.org/10.1038/s41561-025-01818-w
Published:
DOI: https://doi.org/10.1038/s41561-025-01818-w
Share this article
Anyone you share the following link with will be able to read this content:
Sorry, a shareable link is not currently available for this article.
Provided by the Springer Nature SharedIt content-sharing initiative