Abstract
Locating new fossil sites with exceptional soft-tissue preservation is vital for addressing taphonomic bias and accurately reconstructing the fossil record. McGraths Flat, a Miocene rainforest lake Konservat-Lagerstätte, uniquely preserves nanometre-scale soft-tissue structures in laminated Fe-oxyhydroxide (goethite) or ‘ferricrete’. However, constraints on the source of Fe, depositional conditions, and mechanisms that drove the exceptional soft-tissue preservation were lacking. Here, we demonstrate that warm, seasonally wet rainforest conditions generated acidic soils and transported dissolved Fe(II) from weathering basaltic bedrock into an oxbow lake. Fe(III)-oxyhydroxide precipitation then drove fossil burial and mineralization. Our findings suggest that ‘McGraths Flat-type’ fossil preservation may be common and could represent an untapped record of life on land.
| Original language | English |
|---|---|
| Article number | NGS-2024-09-02515 |
| Pages (from-to) | 429-444 |
| Number of pages | 16 |
| Journal | Gondwana Research |
| Volume | 149 |
| DOIs | |
| Publication status | Published - 2026 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 15 Life on Land
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