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Tectonics built Asia's rainforests, but it wasn't alone

Australia's slow crash into Asia helped fill Southeast Asia's forests with species, but new amber fossils suggest the story starts much earlier and is messier than a collision.

Published
November 2, 2026
Reading time
3 min
Categories
Planet & climate

Photo: T. R. Shankar Raman / Wikimedia Commons (CC BY-SA 4.0)

What if the richest forests in Southeast Asia owe more to a continental traffic jam than to the tropical climate we credit for them? The idea is tempting. But the evidence says the real story is subtler than "continent hits continent, forest gets richer", and in our view that subtlety is where the interesting part lives.

A collision that opened a bridge, not a floodgate

The headline claim is simple. As Spektrum puts it, plate tectonics carried animals and plants across oceans, and that is why Southeast Asia's rainforest became especially diverse.

The botanical evidence backs a version of it. A paper on tropical Asian and Australasian floras describes a trans-equatorial migration route that seems to have resulted from the collision of the Australian and Asian plates after the late Oligocene. Giant fossil beans from Indonesian Borneo, from the extinct legume Jantungspermum gunnellii, imply that the ancestors of the black bean tree traveled from Asia to Australia during that collision.

Note the direction of that last one. The traffic did not only flow north. The paper's own title speaks of "asymmetric" migration, which we read as a sign that the exchange was lopsided rather than a one-way delivery of Australian species to Asia.

The amber complicates the tidy tectonic story

Now the twist. Researchers at Curtin University report, as phys.org covers it, that amber fossils reveal how an ancient Australian landmass helped seed Southeast Asia's tropical forests. The specimens come from mid-Cretaceous amber from Kachin, Myanmar, and the study frames a mid-Cretaceous island as a cradle of Southeast Asian plant life. The researchers say the findings challenge the long-held view that the region's diverse flowering-plant ecosystems originated much more recently.

That matters for the thesis. If flowering plants had already diversified that early, then the late collision cannot be the origin of the richness. It looks more like a second act: a bridge that let existing lineages mix, on top of a much older foundation. We would call tectonics a biodiversity engine, but one that runs in several stages, not a single ignition event.

There is also honest uncertainty. The migration paper says "we speculate" that island chains formed after the collision, together with climate change, drove seed plant migrations since the middle Miocene. It adds that biotic dispersal and stable habitat may be crucial. "Speculate" and "may" are the right words here. This is a reconstruction from fossils and distributions, not a recorded event, and we should read headlines about "how Australia enriched Asia" with that in mind.

Deep roots are an argument for protection, not for complacency

What should a reader take from this? First, a skeptical point: a tidy origin story is satisfying but risky. When one dramatic event gets the credit, the quieter ingredients (older lineages, stable habitats, shifting climates) drop out of view. The best reading of the current work, in our opinion, is that the forests are a layered inheritance.

Second, the part of the thesis we fully endorse. If richness took tens of millions of years to assemble, through island chains, dispersal and old refuges, it cannot be rebuilt on a human timescale. Those fossils record a process that took geological time. A cleared forest does not get that time back.

This is where the geology becomes a conservation argument. We tend to defend rainforests for what they do now: carbon, rain, habitat. The fossil record adds a different reason. Many of the lineages there may be survivors of long journeys across oceans and plates, and some may trace back to the Cretaceous. That is a very expensive thing to lose.

We would also be cautious about turning this into a slogan. "Plate tectonics explains biodiversity" is true in the way "rivers explain cities" is true: it names a powerful force and skips everything else. The research cited here points to tectonics, climate, island geography and deep evolutionary history working together.

Our verdict: treat the Australia-Asia collision as a major chapter, not the whole book. Enjoy the idea that continents drifting together seeded forests, then read one level deeper, where Cretaceous amber suggests the book began far earlier. And if the lesson is that diversity has roots this deep, the practical recommendation is plain: protect what remains, because nothing on the planet's calendar can regrow it quickly.

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