Finnegan, Seth

Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity

Payne, J. L., Boyer, A. G., Brown, J. H., Finnegan, S., Kowalewski, M., Krause, R. A., Lyons, S. K., McClain, C. R., McShea, D. W., Novack-Gottshall, P. M., et al. (2009) · Proceedings of the National Academy of Sciences

Evolution and Paleontology StudiesPaleontology and Stratigraphy of Fossils

Cited by 325

Plate tectonic regulation of global marine animal diversity

Zaffos, A., Finnegan, S., & Peters, S. E. (2017) · Proceedings of the National Academy of Sciences

Evolution and Paleontology StudiesPaleontology and Stratigraphy of Fossils

Cited by 214

The evolutionary consequences of oxygenic photosynthesis: a body size perspective

Payne, J. L., McClain, C. R., Boyer, A. G., Brown, J. H., Finnegan, S., Kowalewski, M., Krause, R. A., Lyons, S. K., McShea, D. W., Novack-Gottshall, P. M., et al. (2011) · Photosynthesis Research

Evolution and Paleontology StudiesPhysiological and biochemical adaptations

Cited by 141

CARBONATES IN SKELETON-POOR SEAS: NEW INSIGHTS FROM CAMBRIAN AND ORDOVICIAN STRATA OF LAURENTIA

PRUSS, S. B., FINNEGAN, S., FISCHER, W. W., & KNOLL, A. H. (2010) · PALAIOS

Paleontology and Stratigraphy of FossilsGeological formations and processes

Cited by 139

Carbonate clumped isotope constraints on Silurian ocean temperature and seawater δ18O

Cummins, R. C., Finnegan, S., Fike, D. A., Eiler, J. M., & Fischer, W. W. (2014) · Geochimica et Cosmochimica Acta

Paleontology and Stratigraphy of FossilsGeology and Paleoclimatology Research

Cited by 99