In: Oecologia, 2012, vol. 169, no. 4, p. 939-953
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In: Biodiversity and Conservation, 2008, vol. 17, no. 9, p. 2115-2137
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In: Paläontologische Zeitschrift, 2009, vol. 83, no. 1, p. 207-226
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In: Journal of Paleolimnology, 2008, vol. 40, no. 2, p. 603-618
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In: Marine and Petroleum Geology, 2018, vol. 90, p. 138–148
Deep stratigraphic constrains below the Indonesian Lusi mud eruption are currently lacking due to the absence of deep wells and good quality seismic data. A collection of carbonate clasts has been sampled from the Lusi site, active since its birth in 2006. These specimens are part of a large variety of lithotypes erupted from the main crater. The carbonates analysed comprise scleractinian...
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In: Journal of Paleontology, 2013, vol. 87, no. 5, p. 854-880
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In: Paleoceanography, 2016, vol. 31, no. 3, p. 2015PA002859
Carbonate buildups and mounds are impressive biogenic structures throughout Earth history. In the recent NE Atlantic, cold-water coral (CWC) reefs form giant carbonate mounds of up to 300 m of elevation. The expansion of these coral carbonate mounds is paced by climatic changes during the past 2.7 Myr. Environmental control on their development is directly linked to controls on its main...
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In: Bulletin of the Peabody Museum of Natural History, 2015, vol. 56, no. 2, p. 147–183
The fossil record of the turtle clade Baenidae ranges from the Early Cretaceous (Aptian—Albian) to the Eocene. The group is present throughout North America during the Early Cretaceous, but is restricted to the western portions of the continents in the Late Cretaceous and Paleogene. No credible remains of the clade have been reported outside of North America to date. Baenids were warmadapted...
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In: New Mexico Museum of Natural History & Science bulletin, 2003, no. 23, p. 1-72
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In: Science, 2009, vol. 326, p. 87-93
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