The study reveals that the resemblance arises from how sandy point bars migrate. In meandering rivers without vegetation, these bars often move downstream, leaving deposits that look similar to those from braided rivers. Using standard geological methods, such rivers could easily be misclassified in ancient rock strata.
Lead author Michael Hasson, a PhD student at the Stanford Doerr School of Sustainability, said, "With our study, we're pushing back on the widely accepted story of what landscapes looked like when plant life first evolved on land. We're rewriting the story of the intertwined relationship between plants and rivers, which is a significant revision to our understanding of the history of the Earth."
The team analyzed nearly 4,500 river bends in 49 rivers worldwide, comparing vegetated and unvegetated systems. They confirmed that vegetation alters the trajectory of point bar migration, shifting their growth laterally instead of downstream. This difference explains why previous interpretations tied the emergence of meanders to plants.
Senior author Mathieu Lapotre noted, "In our paper, we show that this conclusion - which is taught in all geology curricula to this day - is most likely incorrect." By reexamining modern rivers, the team demonstrated that unvegetated meanders would be miscategorized as braided if studied solely by bar trajectory in rock layers.
The findings suggest carbon-rich floodplains from meandering rivers likely formed much earlier and more widely than previously assumed. Since these floodplains act as long-term carbon reservoirs, the work carries implications for reconstructing ancient carbon cycles and refining climate models.
Hasson emphasized, "Understanding how our planet is going to respond to human-induced climate change hinges on having an accurate baseline for how it has responded to past perturbations. The rock record provides that baseline, but it's only useful if we interpret it accurately."
Research Report:Vegetation changes the trajectory of river bends
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