Abstract
Hypersaline environments are commonly assumed to be barren of metazoans and therefore are avoided by paleontologists, yet a number of early Paleozoic jawless vertebrate groups specialized to live in such settings. Sampling bias against restricted settings resulted in substantial underestimation of their diversity. Rare studies venturing into such environments yielded multiple new species of conodonts, suggesting that the diversity and habitat range of these hyperdiverse predators of the early oceans are equally underestimated. We describe here autochthonous conodont fauna from evaporite-bearing horizons from the middle Silurian of Estonia that provide evidence for efficient osmoregulation in this group. Based on a global compilation of coeval conodont assemblages, we show that marginal-marine, periodically emergent environments were characterized by higher conodont diversity than open-marine shallow settings. This diversity is due to a high number of species occurring in these environments only. The high degree of specialization is also reflected by the highest within-habitat variability (β diversity) in marginal settings. Most conodont species had narrow environmental niches and, unlike in marine invertebrates, extreme environments were inhabited by the most specialized taxa. Such environments represent a large proportion of early Paleozoic tropical epicratonic basins. Our analysis allows quantification of the degree to which mid-Silurian conodont diversity is underestimated as a result of sampling bias against marginal-marine settings.
Original language | English |
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Pages (from-to) | 3-6 |
Number of pages | 4 |
Journal | Geology |
Volume | 45 |
Issue number | 1 |
DOIs | |
Publication status | Published - 2017 |
Bibliographical note
Funding Information:This work was supported by the German Research Foundation (Project Mu 2352/3). Jarochowska received support from SYNTHESYS, which is financed by the European Community-Research Infrastructure Action under the Seventh Framework Programme (FP7/2007-2013). We thank W. Kiessling and K. De Baets for discussions; C. Krause for help with data compilation; C. Schulbert, O. Hints, and P. Tonarová for assistance in microscopy; and reviewers J.E. Barrick, I. Percival, and J. Sanz-López for constructive comments. This is Paleobiology Database publication 269.
Publisher Copyright:
© 2016 Geological Society of America.
Funding
This work was supported by the German Research Foundation (Project Mu 2352/3). Jarochowska received support from SYNTHESYS, which is financed by the European Community-Research Infrastructure Action under the Seventh Framework Programme (FP7/2007-2013). We thank W. Kiessling and K. De Baets for discussions; C. Krause for help with data compilation; C. Schulbert, O. Hints, and P. Tonarová for assistance in microscopy; and reviewers J.E. Barrick, I. Percival, and J. Sanz-López for constructive comments. This is Paleobiology Database publication 269.