File:Feart-08-00098-g001.jpg

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English: Figure 1. The geological and morphological history of horseshoe crabs across the Phanerozoic. Number of named species is presented as well as suggested palaeoenvironment (Tables 1–7). A major transition to freshwater conditions occurred between the Devonian and Carboniferous. This was concurrent with a decrease in synziphosurine taxa and an increase in xiphosurids. Limulids had a diversification event in the Triassic and there was a transition back to dominantly marine conditions in the Jurassic. Dashed lines represent ghost lineages.
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Source https://www.frontiersin.org/articles/10.3389/feart.2020.00098/full
Author Russell D. C. Bicknell and Stephen Pates

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current23:13, 30 June 2022Thumbnail for version as of 23:13, 30 June 20221,220 × 1,600 (819 KB)Qohelet12 (talk | contribs)Uploaded a work by Russell D. C. Bicknell and Stephen Pates from https://www.frontiersin.org/articles/10.3389/feart.2020.00098/full with UploadWizard

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