Year |
Citation |
Score |
2019 |
Pietsch C, Ritterbush KA, Thompson JR, Petsios E, Bottjer DJ. Evolutionary models in the Early Triassic marine realm Palaeogeography, Palaeoclimatology, Palaeoecology. 513: 65-85. DOI: 10.1016/J.Palaeo.2017.12.016 |
0.526 |
|
2019 |
Petsios E, Thompson JR, Pietsch C, Bottjer DJ. Biotic impacts of temperature before, during, and after the end-Permian extinction: A multi-metric and multi-scale approach to modeling extinction and recovery dynamics Palaeogeography, Palaeoclimatology, Palaeoecology. 513: 86-99. DOI: 10.1016/J.Palaeo.2017.08.038 |
0.433 |
|
2018 |
Ivany LC, Pietsch C, Handley JC, Lockwood R, Allmon WD, Sessa JA. Little lasting impact of the Paleocene-Eocene Thermal Maximum on shallow marine molluscan faunas. Science Advances. 4: eaat5528. PMID 30191179 DOI: 10.1126/Sciadv.Aat5528 |
0.518 |
|
2016 |
Pietsch C, Harrison HC, Allmon WD. Whence the Gosport Sand (Upper Middle Eocene, Alabama)? The Origin of Glauconitic Shell Beds In the Paleogene of the U.S. Gulf Coastal Plain Journal of Sedimentary Research. 86: 1249-1268. DOI: 10.2110/Jsr.2016.72 |
0.512 |
|
2016 |
Pietsch C, Petsios E, Bottjer DJ. Sudden and extreme hyperthermals, low-oxygen, and sediment influx drove community phase shifts following the end-Permian mass extinction Palaeogeography, Palaeoclimatology, Palaeoecology. 451: 183-196. DOI: 10.1016/J.Palaeo.2016.02.056 |
0.424 |
|
2014 |
Pietsch C, Mata SA, Bottjer DJ. High temperature and low oxygen perturbations drive contrasting benthic recovery dynamics following the end-Permian mass extinction Palaeogeography, Palaeoclimatology, Palaeoecology. 399: 98-113. DOI: 10.1016/J.Palaeo.2014.02.011 |
0.47 |
|
2014 |
Pietsch C, Bottjer DJ. The importance of oxygen for the disparate recovery patterns of the benthic macrofauna in the Early Triassic Earth-Science Reviews. 137: 65-84. DOI: 10.1016/J.Earscirev.2013.12.002 |
0.46 |
|
2010 |
Pietsch C, Bottjer DJ. Comparison of changes in ocean chemistry in the early triassic with trends in diversity and ecology Journal of Earth Science. 21: 147-150. DOI: 10.1007/S12583-010-0195-9 |
0.438 |
|
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