Karst greening faces a hidden limit: Too little soil
Peer-Reviewed Publication
Updates every hour. Last Updated: 21-Oct-2026 21:17 ET (22-Oct-2026 01:17 GMT/UTC)
A synthesis of ground surveys across Southwest China finds that soil thickness explains nearly 70% of the spatial variation in woody vegetation growth potential, far more than climate or soil nutrient concentrations. Below a 57.5-centimeter threshold, limited soil volume becomes the dominant constraint, where vegetation becomes less related to soil nutrient concentrations and more closely associated with climate variability.
f you want to know how rapidly pumping carbon dioxide into the atmosphere will impact future forest ecosystems, you have to look into the distant past. The researchers behind a new study published in Science have done just that, reconstructing the forest canopy of 56 million years ago, during a massive and abrupt emission of carbon into the atmosphere during the Paleocene-Eocene Thermal Maximum (PETM). For the first time, the authors of the study used fossilized leaf cells to reconstruct the tree canopy of the PETM, Earth’s most recent period of comparable global warming, with chilling implications for our near future. The authors found that the PETM was marked by a widespread browning of Earth's landscapes. Against a backdrop of elevated atmospheric CO₂, global warming, and reduced rainfall triggered by volcanically driven carbon release, plant species migrated northwards, and canopy cover declined, accelerating erosion and disrupting the terrestrial water cycle. The human-caused climate change happening now is pumping CO2 at an order of magnitude faster than the ancient parallel. Trees are at the root of these drastic changes.
Forest fossils from Wyoming suggest that rapid and prolonged greenhouse warming during the Paleocene–Eocene Thermal Maximum (PETM) caused forests to thin, drastically reshaped plant communities, and reduced overall vegetation carbon storage. The findings could foreshadow challenges facing modern forests in our rapidly warming world. Although rising atmospheric carbon dioxide initially stimulated plant growth across much of the globe, that trend has reversed in recent decades as increasing heat and drought place growing stress on vegetation. This shift raises concerns that forests may lose their capacity to store carbon, thereby accelerating climate change. However, the long-term effects of sustained greenhouse warming on forest structure and carbon storage remain poorly understood, leaving uncertainty about the future of today's forests in our warming world.
To understand how forests respond to prolonged atmospheric warming, Regan Dunn and colleagues examined fossil evidence from Wyoming’s Hanna Basin. They wanted to know how forests responded to extreme greenhouse warming during the PETM – often considered one of the closest natural analogs to modern human-driven climate change – about 56 million years ago. By combining fossil pollen, sediment records, geochemical data, and a new proxy for reconstructing Leaf Area Index (LAI) from fossil leaf cuticles, Dunn et al. reconstructed changes in plant communities and vegetation structure during this period of rapid carbon release and global warming. Dunn et al. found that PETM warming caused rapid forest canopy opening, increased landscape erosion, and major shifts in forest composition, including the replacement of temperate broad-leaved angiosperm plants with more heat-tolerant species, such as palms and ferns. The findings show that prolonged warming can reduce forest density and carbon storage, even when elevated carbon dioxide initially promotes plant growth, offering insight into how modern forests may respond as rising temperatures and drought increasingly threaten their ability to absorb and store carbon.