File:Feart-08-00098-g001.jpg
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[edit]DescriptionFeart-08-00098-g001.jpg |
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. |
Date | |
Source | https://www.frontiersin.org/articles/10.3389/feart.2020.00098/full |
Author | Russell D. C. Bicknell and Stephen Pates |
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current | 23:13, 30 June 2022 | 1,220 × 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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Software used | Adobe Photoshop CS6 (Windows) |
File change date and time | 17:24, 4 July 2020 |
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Date and time of digitizing | 20:23, 20 May 2020 |
Date metadata was last modified | 22:54, 4 July 2020 |
Unique ID of original document | xmp.did:FBCBD6E3ECBDEA11AA30A64290C96313 |
IIM version | 31,829 |
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