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Publications
2011
Linguliform Brachiopods from the Terminal Cambrian and Lowest Ordovician of the Oaxaquia Microcontinent (Southern Mexico). Journal of Paleontology 85, 122-155. doi:10.1666/10-074.1
, 2011. , 2011.
Left Behind--Delayed Extinction and a Relict Trilobite Fauna in the Cambrian--Ordovician Boundary Succession (East Laurentian Platform, New York). Geological Magazine 148, 529-557. doi:10.1017/S0016756810000919
, 2011. Tremadocian (Lower Ordovician) Biotas and Sea-level Changes on the Avalon Microcontinent. Journal of Paleontology 85, 680-696. doi:10.1666/10-076.1
, 2011. The Lawsonian Stage - the Eoconodontus Notchpeakensis FAD and HERB Carbon Isotope Excursion Define a Globally Correlatable Terminal Cambrian Stage. Bulletin of Geosciences 86, 621-640. doi:10.3140/bull.geosci.1251
, 2011. Proterozoic Phytoplankton and Timing of Chlorophyte Algae Origins. Palaeontology 54, 721-733. doi:10.1111/j.1475-4983.2011.01054.x
, 2011. 2010
First Evidence for Cambrian Glaciation Provided by Sections in Avalonian New Brunswick and Ireland--Additional Data for Avalon-Gondwana Separation by the Earliest Palaeozoic. Palaeogeography, Palaeoclimatology, Palaeoecology 285, 174-185. doi:10.1016/j.palaeo.2009.11.009
, 2010. Early Ordovician Community Evolution with Eustatic Change Through the Middle Beekmantown Group, Northeast Laurentia. Palaeogeography, Palaeoclimatology, Palaeoecology 294, 174-188. doi:10.1016/j.palaeo.2009.11.025
, 2010. Cambrian Origin of All Skeletalized Metazoan Phyla--Discovery of Earth's Oldest Bryozoans (Upper Cambrian, Southern Mexico). Geology 38, 547-550. doi:10.1130/G30870.1
, 2010. When the Phyla Came Marching In: Modern Marine Organisms Originate in the Cambrian Period. Legacy: The Magazine of the New York State Museum 6, 9.
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