Turnover from mollusk-dominated Depauperate Zone (late Ordovician) to brachiopod-dominated (early Silurian) faunas in central North America
Author:
Affiliation:
1. Department of Geosciences, Williams College, Williamstown, MS 01267, USA;
Publisher
Informa UK Limited
Subject
Paleontology,Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/11035897.2013.838997
Reference17 articles.
1. Late Ordovician–Early Silurian δ13C chemostratigraphy in the Upper Mississippi Valley: implications for chronostratigraphy and depositional interpretations
2. The Palaeozoic geography of Laurentia and western Laurussia: A stable craton with mobile margins
3. Frest, T.J., Brett, C.E. & Witzke, B.J., 1999: Caradocian-Gedinnian echinoderm associations of Central and Eastern North America. In A.J.Boucot & J.D.Lawson (eds.): Paleocommunities: a case study from the Silurian and Lower Devonian, 638–783. Cambridge University Press, Cambridge.
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