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Peter Scogings

pnas.org/doi/10.1073/pnas.2311

The authors provide evidence that vegetation changes in SE Asia during the Last Glacial Maximum involved "fluid" transitions between lowland rainforest, seasonally dry forest and tropical montane forest, not switches between forest and savanna. However, their depiction of the alternative stable state model of forests and savannas is flawed. It doesn't consider recent insights and is based on erroneous interpretation of earlier studies in .