File:Bows and Unicorns Quarry bonebed development.png

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Four key pre-diagenetic stages interpreted for RUQ bonebed development.

(A) Deposition of vertebrate and other fossils in the context of a low energy lake setting. (B) Lowering of water table and colonization of the former lake area by plants, accompanied by formation of pedogenic carbonate nodules at and below the bone layer. (C) Lower temperature fire event creating hydraulic instability in the region. (D) Avulsion of nearby river channel leading to exhumation and reburial of the former lake and floodplain fossils into a channel setting.
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Source https://peerj.com/articles/11013/
Author Alan L. Titus​1, Katja Knoll1, Joseph J.W. Sertich2, Daigo Yamamura3, Celina A. Suarez3, Ian J. Glasspool4, Jonathan E. Ginouves1, Abigail K. Lukacic1, Eric M. Roberts5

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current15:49, 22 April 2021Thumbnail for version as of 15:49, 22 April 20212,437 × 2,828 (1.04 MB)FunkMonk (talk | contribs){{Information |description=Four key pre-diagenetic stages interpreted for RUQ bonebed development. (A) Deposition of vertebrate and other fossils in the context of a low energy lake setting. (B) Lowering of water table and colonization of the former lake area by plants, accompanied by formation of pedogenic carbonate nodules at and below the bone layer. (C) Lower temperature fire event creating hydraulic instability in the region. (D) Avulsion of nearby river channel leading to exhumation and...

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