Vidas, Davor
5 papers on CoChatORCID 0000-0001-8134-7425
Most cited papers
- Verified
The Anthropocene is functionally and stratigraphically distinct from the Holocene
Waters, C. N., Zalasiewicz, J., Summerhayes, C., Barnosky, A. D., Poirier, C., Gałuszka, A., Cearreta, A., Edgeworth, M., Ellis, E. C., Ellis, M., et al. (2016) · Science
Geology and Paleoclimatology ResearchPaleontology and Stratigraphy of Fossils
Cited by 2,375
- Verified
When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal
Zalasiewicz, J., Waters, C. N., Williams, M., Barnosky, A. D., Cearreta, A., Crutzen, P., Ellis, E., Ellis, M. A., Fairchild, I. J., Grinevald, J., et al. (2015) · Quaternary International
Geology and Paleoclimatology ResearchPaleontology and Stratigraphy of Fossils
Cited by 784
- Verified
The Working Group on the Anthropocene: Summary of evidence and interim recommendations
Zalasiewicz, J., Waters, C. N., Summerhayes, C. P., Wolfe, A. P., Barnosky, A. D., Cearreta, A., Crutzen, P., Ellis, E., Fairchild, I. J., Gałuszka, A., et al. (2017) · Anthropocene
Geology and Paleoclimatology ResearchPaleontology and Stratigraphy of Fossils
Cited by 487
- Verified
The Anthropocene: a conspicuous stratigraphical signal of anthropogenic changes in production and consumption across the biosphere
Williams, M., Zalasiewicz, J., Waters, C. N., Edgeworth, M., Bennett, C., Barnosky, A. D., Ellis, E. C., Ellis, M. A., Cearreta, A., Haff, P. K., et al. (2016) · Earth's Future
Paleontology and Stratigraphy of FossilsEarth Systems and Cosmic Evolution
Cited by 91
- Verified
Colonization of the Americas, ‘Little Ice Age’ climate, and bomb-produced carbon: Their role in defining the Anthropocene
Members of the Anthropocene Working Group:, Zalasiewicz, J., Waters, C. N., Barnosky, A. D., Cearreta, A., Edgeworth, M., Ellis, E. C., Gałuszka, A., Gibbard, P. L., Grinevald, J., et al. (2015) · The Anthropocene Review
Geology and Paleoclimatology ResearchArchaeology and ancient environmental studies
Cited by 82
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