Double stress of waterlogging and drought drives forest–savanna coexistence
Open accessAbstract
Forest–savanna boundaries are ecotones that support complex ecosystem functions and are sensitive to biotic/abiotic perturbations. What drives their distribution today and how it may shift in the future are open questions. Feedbacks among climate, fire, herbivory, and land use are known drivers. Here, we show that alternating seasonal drought and waterlogging stress favors the dominance of savanna-like ecosystems over forests. We track the seasonal water-table depth as an indicator of water stress when too deep and oxygen stress when too shallow and map forest/savanna occurrence within this double-stress space in the neotropics. We find that under a given annual precipitation, savannas are favored in landscape positions experiencing double stress, which is more common as the dry season strengthens (climate driver) but only found in waterlogged lowlands (terrain driver). We further show that hydrological changes at the end of the century may expose some flooded forests to savanna expansion, affecting biodiversity and soil carbon storage. Our results highlight the importance of land hydrology in understanding/predicting forest–savanna transitions in a changing world.
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Although these ecosystem transitions have been confirmed only in the Negro river basin, floodplain forests in other parts of the Amazon were shown to be particularly vulnerable to collapse.
“Although these ecosystem transitions have been confirmed only in the Negro river basin (central Amazon), floodplain forests in other parts of the Amazon were shown to be particularly vulnerable to collapse45,64,65.”
From Critical transitions in the Amazon forest system (2024) · cites this paper as [64]
In “Future Changes in Double Stress,” the paper says floodplain forests of the Amazonas, Madeira, and Upper Negro Rivers are particularly affected by simulated hydrologic stress, supporting the geographic point. It does not establish that those forests are particularly vulnerable to collapse: the same section says vegetation shifts depend on local factors and that more research is needed to determine each forest type’s vulnerability. (LLM, conf=0.86)
Experimental — accuracy not yet measuredOther key heterogeneity factors include topography, which determines plant access to groundwater, and seasonal flooding, which increases forest vulnerability to wildfires.
“Other key heterogeneity factors (Extended Data Fig. 6) include topography, which determines plant access to groundwater64, and seasonal flooding, which increases forest vulnerability to wildfires65.”
From Critical transitions in the Amazon forest system (2024) · cites this paper as [64]
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Nepstad, D. C., Stickler, C. M., Filho, B. S., & Merry, F. (2008) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2007.0036 · Cited by 725 · see citing works
(2014) · Climate Change 2013 – The Physical Science Basis · doi:10.1017/cbo9781107415324.026 · Cited by 342 · see citing works
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Research works printed but not linked: 35
- [1]M. Hirota, M. Holmgren, E. H. V. Nes, M. Scheffer, Global resilience of tropical forest and savanna to critical transitions. Science 334, 232– 235 (2011). 21998390
- [2]A. C. Staver, S. Archibald, S. A. Levin, The global extent and determinants of savanna and forest as alternative biome states. Science 334, 230– 232 (2011). 21998389
- [3]I. Oliveras, Y. Malhi, Many shades of green: The dynamic tropical forest–savannah transition zones. Philos. Trans. R. Soc. B 371, 20150308 (2016). PMC4978866 27502373
- [4]A. C. Staver, S. Archibald, S. Levin, Tree cover in sub-Saharan Africa: Rainfall and fire constrain forest and savanna as alternative stable states. Ecology 92, 1063– 1072 (2011). 21661567
- [5]G. Miguez-Macho, Y. Fan, Spatiotemporal origin of soil water taken up by vegetation. Nature 598, 624– 628 (2021). 34616038
- [6]Y. Fan, G. Miguez-Macho, E. G. Jobbágy, R. B. Jackson, C. Otero-Casal, Hydrologic regulation of plant rooting depth. Proc. Natl. Acad. Sci. U.S.A. 114, 10572– 10577 (2017). 28923923 PMC5635924
- [7]P. Parolin, Morphological and physiological adjustments to waterlogging and drought in seedlings of Amazonian floodplain trees. Oecologia 128, 326– 335 (2001). 24549901
- [9]Y. N. Araya, A fundamental, eco-hydrological basis for niche segregation in plant communities. New Phytol. 189, 253– 258 (2011). 20868394
- [16]Y. Fan, H. Li, G. Miguez-Macho, Global patterns of groundwater table depth. Science 339, 940– 943 (2013). 23430651
- [19]P. Parolin, F. Wittmann, Struggle in the flood: Tree responses to flooding stress in four tropical floodplain systems. AoB Plants 2010, plq003 (2010). 22476061 PMC2965040
- [20]Y. N. Pokhrel, Y. Fan, G. Miguez-Macho, Potential hydrologic changes in the Amazon by the end of the 21st century and the groundwater buffer. Environ. Res. Lett. 9, 084004 (2014).
- [24]F. R. C. Costa, J. Schietti, S. C. Stark, M. N. Smith, The other side of tropical forest drought: Do shallow water table regions of Amazonia act as large-scale hydrological refugia from drought? New Phytol. 237, 714– 733 (2022). 35037253
- [25]R. C. Rivaben, Do fire and flood interact to determine forest islet structure and diversity in a Neotropical wetland? Flora 281, 151874 (2021).
- [26]B. M. Flores, Floodplains as an Achilles’ heel of Amazonian forest resilience. Proc. Natl. Acad. Sci. U.S.A. 114, 4442– 4446 (2017). 28396440 PMC5410816
- [28]G. Sarmiento, “ The Savannas of tropical America” in En: Tropical savannas, F. Bourliere, Ed. (Elsevier, Amsterdam, NL, 1983), pp. 245– 288.
- [32]R. S. Oliveira, Linking plant hydraulics and the fast–slow continuum to understand resilience to drought in tropical ecosystems. New Phytol. 230, 904– 923 (2021). 33570772
- [33]M. Bustamante, Potential impacts of climate change on biogeochemical functioning of Cerrado ecosystems. Braz. J. Biol. 72, 655– 671 (2012). 23011296
- [35]P. A. Furley, “ Edaphic changes at the forest-savanna boundary with particular reference to the neotropics” in Nature and Dynamics of Forest-Savanna Boundaries, P. A. Furley, J.Proctor, J. A. Ratter, Eds. (CRC Press, London, 1992).
- [39]R. de O. Xavier, M. B. Leite, K. Dexter, D. M. da Silva Matos, Differential effects of soil waterlogging on herbaceous and woody plant communities in a Neotropical savanna. Oecologia 190, 471– 483 (2019). 31129717
- [40]M. D. Oyama, C. A. Nobre, A new climate-vegetation equilibrium state for Tropical South America: A new climate-vegetation state. Geophys. Res. Lett. 30, 2199 (2003).
- [42]Y. Malhi, Exploring the likelihood and mechanism of a climate-change-induced dieback of the Amazon rainforest. Proc. Natl. Acad. Sci. U.S.A. 106, 20610– 20615 (2009). 19218454 PMC2791614
- [43]M. T. Coe, Deforestation and climate feedbacks threaten the ecological integrity of south–southeastern Amazonia. Philos. Trans. R. Soc. Lond. B Biol. Sci. 368, 20120155 (2013). 23610166 PMC3638426
- [44]J. V. Tavares, Basin-wide variation in tree hydraulic safety margins predicts the carbon balance of Amazon forests. Nature 617, 111– 117 (2023). 37100901 PMC10156596
- [45]D. C. Zemp, Self-amplified Amazon forest loss due to vegetation-atmosphere feedbacks. Nat. Commun. 8, 14681 (2017). 28287104 PMC5355804
- [47]F. M. Sabatini, Global patterns of vascular plant alpha diversity. Nat. Commun. 13, 4683 (2022). 36050293 PMC9436951
- [48]F. C. Draper, The distribution and amount of carbon in the largest peatland complex in Amazonia. Environ. Res. Lett. 9, 124017 (2014).
- [50]A. A. Alencar, P. M. Brando, G. P. Asner, F. E. Putz, Landscape fragmentation, severe drought, and the new Amazon forest fire regime. Ecol. Appl. 25, 1493– 1505 (2015). 26552259
- [51]S. E. Page, The amount of carbon released from peat and forest fires in Indonesia during 1997. Nature 420, 61– 65 (2002). 12422213
- [56]E. H. van Nes, M. Hirota, M. Holmgren, M. Scheffer, Tipping points in tropical tree cover: Linking theory to data. Glob. Change Biol. 20, 1016– 1021 (2014). 24106057
- [57]C. DiMiceli, MOD44B MODIS/Terra vegetation continuous fields yearly L3 global 250m SIN grid V006. (2015). 10.5067/MODIS/MOD44B.006. 12 November 2021. · DOI
- [58]C. M. Souza, Reconstructing three decades of land use and land cover changes in Brazilian biomes with landsat archive and earth engine. Remote Sens. 12, 2735 (2020).
- [61]B. Lehner, K. Verdin, A. Jarvis, New global hydrography derived from spaceborne elevation data. Eos, Transactions, American Geophysical Union, 89, 93– 94, 10.1029/2008eo100001 (2008). · DOI · Paper page
- [62]C. Dimiceli, M. Carroll, R. Sohlberg, D. H. Kim, M. Kelly, MOD44B MODIS/terra vegetation continuous fields yearly L3 global 250m SIN grid V006. NASA EOSDIS Land Processes DAAC. 10.5067/MODIS/MOD44B.006. Accessed 20 March 2022. · DOI
- [63]C. M. Souza, Reconstructing Three Decades of Land Use and Land Cover Changes in Brazilian Biomes with Landsat Archive and Earth Engine. Remote Sens, 12, 10.3390/rs12172735 (2020). · DOI
- [66]C. R. C. Mattos, Data for “Double stress of waterlogging and drought drives forest–savanna coexistence.” Zenodo. https://zenodo.org/record/7950934. Deposited 20 May 2023. PMC10438376 37549286
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Critical transitions in the Amazon forest system
Flores, B. M., Montoya, E., Sakschewski, B., Nascimento, N., Staal, A., Betts, R. A., Levis, C., Lapola, D. M., Esquível-Muelbert, A., Jakovac, C., et al. (2024) · Nature · doi:10.1038/s41586-023-06970-0 · Cited by 607 · see citing works
Self-citation
- Authors
- Mattos, C. R. C., Hirota, M., Oliveira, R. S., Flores, B. M., Miguez-Macho, G., Pokhrel, Y., & Fan, Y.
- Affiliations
- Rutgers, The State University of New Jersey (US)
- Universidade Estadual de Campinas (UNICAMP) (BR)
- Universidade Federal de Santa Catarina (BR)
- CRETUS, Non-Linear Physics Group, Faculty of Physics, Universidade de Santiago de Compostela, Santiago de Compostela 15782, Spain
- Michigan State University (US)
- Corresponding author
- Mattos, Caio R. C.
- Venue
- Proceedings of the National Academy of Sciences
- Publisher
- National Academy of Sciences
- Published
- 2023-08-07
- Volume
- 120
- Issue
- 33
- Pages
- e2301255120-e2301255120
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- PMC
- PMC10438376
- OpenAlex
- W4385618075
- Cited by
- 51
- References
- 2
- Citations by year
- 2026: 16 · 2025: 13 · 2024: 16 · 2023: 6
- FWCI
- 5.27
- Type
- journal article
- Language
- en
- Open access
- hybrid
- doi.org
- Licence
- Locations
- Proceedings of the National Academy of Sciences (publishedVersion, cc-by-nc-nd)
- PubMed Central (publishedVersion, cc-by-nc-nd)
- PubMed (publishedVersion)
- Funders
- NSF | GEO | Division of Earth Sciences (825813, 1752729)
- NSF | GEO | Division of Atmospheric and Geospace Sciences (185270)
- Instituto Serrapilheira (1709-18983)
- FAPESP-NERC (2019-07773-1)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Ecosystem dynamics and resilience
- Physical Sciences › Environmental Science › Global and Planetary Change › Plant Water Relations and Carbon Dynamics
- Physical Sciences › Environmental Science › Ecology › Plant Ecology and Soil Science
- Keywords
- flooding stress, drought stress, water table depth, oxygen stress, savanna expansion, land surface hydrology, flooded forest, Neotropical forests, climate change impacts, soil carbon storage, ecosystem transitions
- MeSH terms
- Climate, Trees, Ecosystem, Droughts, Forests, Grassland
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