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| Content Provider | Springer Nature Link |
|---|---|
| Author | Huyghe, Damien Merle, Didier Lartaud, Franck Cheype, Emilie Emmanuel, Laurent |
| Copyright Year | 2012 |
| Abstract | The present study reports the evolution of environmental conditions and seawater temperatures during the establishment of a marine hotspot of paleobiodiversity that took place in the Paris Basin during the Lutetian. The stable isotope compositions (δ18O and δ13C) of three species of molluscs (two bivalves: Cubitostrea plicata and Venericardia imbricata, and one gastropod: Sigmesalia multisulcata) collected along the reference section of Grignon (Falunière) are used for paleoenvironmental and paleoclimatic reconstructions. Additional high-resolution analyses on one specimen of Haustator imbricatarius allow the documentation of seasonal changes for temperature. The high-resolution profiles of the δ18O signatures of S. multisulcata reveal that these gastropods mineralized their shell during the warm months of the year, as did V. imbricata, which probably had a short life span (less than 1 year). These two species thus only yield temperatures for the summer period, from 22 to 30 °C. The δ18O of C. plicata shells indicate mean annual sea surface temperatures ranging between 15 and 23 °C during the Middle Lutetian, with minimal temperatures probably reflecting greater depth at the base of the section. The seasonal contrasts reconstructed in the upper part of the section, from the large gastropod H. imbricatarius, ranged between 18 and 30 °C. Comparison of the isotopic values of the species indicates that the δ13C of the three taxa seems to be mostly influenced by ecological features, leading to differences between endobenthic (V. imbricata) and epibenthic species (C. plicata); or the food habits. The paleoclimatic reconstructions show that the Lutetian climate was relatively stable in the Paris Basin with long-term cooling of the mean annual sea-surface temperatures. Nevertheless, this study shows that despite a context of colder conditions compared to the Early Eocene, the climate provided a favorable context for the increase of marine biodiversity in the Paris Basin during the Middle Lutetian. |
| Starting Page | 587 |
| Ending Page | 604 |
| Page Count | 18 |
| File Format | |
| ISSN | 01729179 |
| Journal | Facies |
| Volume Number | 58 |
| Issue Number | 4 |
| e-ISSN | 16124820 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2012-04-18 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Lutetian Paris Basin Molluscs Climate Stable isotopes Paleobiodiversity Ecology Geochemistry Paleontology Biogeosciences Sedimentology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geology Stratigraphy Paleontology |
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