Embolism resistance supports the contribution of dry-season precipitation to transpiration in eastern Amazon forests

Transpiration drives most of the local rainfall during the dry season in the Amazon forests by recycling moisture into the atmosphere. However, the source, temporal origin of transpiration, and spatial distribution of transpiration water sources remain unclear. Here, we quantify transpiration sources across a topographic gradient in the eastern Amazon. We show that on hills, dry-season transpiration sources are mostly shallow soil water recharged by dry-season rainfall. This is different in valleys, where tree water sources include both shallow and deep soil layers, with both dry- and wet-season contributions. We show that species embolism resistance largely explains this pattern in tree water use but with contrasting trade-offs between topographic positions. The significant relationship between embolism resistance and depth of water uptake in both hill and valley species may merit incorporation into process-based models to understand changes in vegetation and land surface fluxes.

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Publication Details

Journal
Proceedings of the National Academy of Sciences
Published
2025-08-14
DOI
https://doi.org/10.1073/pnas.2501585122
Citations
3
Primary Topic
Environmental and biological studies
Type
article
Field-Weighted Citation Impact
5.15
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article

Embolism resistance supports the contribution of dry-season precipitation to transpiration in eastern Amazon forests

Mayda Rocha, Caio R. C. Mattos, Gleicy Rodrigues, Rafael S. Oliveira et al.
3 citations
Proceedings of the National Academy of Sciences
Environmental and biological studies
5.15
article

Embolism resistance supports the contribution of dry-season precipitation to transpiration in eastern Amazon forests

Mayda Rocha, Caio R. C. Mattos, Gleicy Rodrigues, Rafael S. Oliveira, Leandro Lacerda Giacomin, Marina Hirota, Monique Bohora Schlickmann, Jeffrey J. McDonnell, Ying Fan, Magali F. Nehemy, Deliane Penha, Julliene S G M Silva
article en
3 citations

Abstract

Transpiration drives most of the local rainfall during the dry season in the Amazon forests by recycling moisture into the atmosphere. However, the source, temporal origin of transpiration, and spatial distribution of transpiration water sources remain unclear. Here, we quantify transpiration sources across a topographic gradient in the eastern Amazon. We show that on hills, dry-season transpiration sources are mostly shallow soil water recharged by dry-season rainfall. This is different in valleys, where tree water sources include both shallow and deep soil layers, with both dry- and wet-season contributions. We show that species embolism resistance largely explains this pattern in tree water use but with contrasting trade-offs between topographic positions. The significant relationship between embolism resistance and depth of water uptake in both hill and valley species may merit incorporation into process-based models to understand changes in vegetation and land surface fluxes.

Proceedings of the National Academy of SciencesVol. 122(33)
Rutgers, The State University of New Jersey (US), Planetary Science Institute (US), Universidade Federal do Oeste do Pará (BR), Universidade Federal da Paraíba (BR), Universidade Estadual de Campinas (UNICAMP) (BR), University of Trento (IT), North China University of Water Resources and Electric Power (CN), University of Saskatchewan (CA), University of Florida (US), Universidade Federal de Santa Catarina (BR), Rutgers Sexual and Reproductive Health and Rights (NL), Institute of Plant Biology (HU), Trent University (CA), University of Birmingham (GB), Okanagan University College (CA)
Openalex Percentile: Top 5%
Environmental and biological studies
5.15
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