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Transient dwarfism of soil fauna during the Paleocene–Eocene Thermal Maximum
Soil organisms, as recorded by trace fossils in paleosols of the Willwood Formation, Wyoming, show significant body-size reductions and increased abundances during the Paleocene–Eocene Thermal Maximum (PETM). Paleobotanical, paleopedologic, and oxygen isotope studies indicate high temperatures durin...
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| Hoofdauteurs: | , , , |
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| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
National Academy of Sciences
2009
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2757401/ https://ncbi.nlm.nih.gov/pubmed/19805060 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0909674106 |
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