In: Swiss Journal of Geosciences, 2018, vol. 111, no. 3, p. 523–536
Large benthic foraminifera are important components of tropical shallow water carbonates. Their structure, developed to host algal symbionts, can be extremely elaborate and presents stratigraphically-significant evolutionary patterns. Therefore their distribution is important in biostratigraphy, especially in the Indo-Pacific area. To provide a reliable age model for two intervals of IODP...
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In: Swiss Journal of Geosciences, 2018, vol. 111, no. 3, p. 561–572
Cold-water coral ecosystems represent unique and exceptionally diverse environments in the deep-sea. They are well developed along the Irish margin, varying broadly in shape and size. The Moira Mounds, numerous small-sized mounds, are nestled in the Belgica Mound Province (Porcupine Seabight, North-East Atlantic). The investigation of living (Rose Bengal stained) and dead benthic...
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In: Newsletters on Stratigraphy, 2018, vol. 51, no. 3, p. 343–380
The upper Cenomanian – lower Turonian is a key-stratigraphic interval, as it encompasses the Late Cretaceous supergreenhouse and a major perturbation of the global carbon cycle (i. e., Oceanic Anoxic Event 2) as evidenced by a global positive carbon isotope excursion and by the nearly world-wide deposition of organic-rich marine facies. A turnover in planktonic foraminiferal assemblages and...
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In: Coral Reefs, 2007, vol. 26, no. 4, p. 867-882
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 2, p. 215-225
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In: Oecologia, 2007, vol. 152, no. 2, p. 265-273
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In: Biodiversity and Conservation, 2008, vol. 17, no. 2, p. 317-328
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In: Marine Biology, 2008, vol. 153, no. 5, p. 899-906
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In: Eclogae Geologicae Helvetiae, 2006, vol. 99, no. 3, p. 295-299
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In: Plant Ecology, 2005, vol. 176, no. 2, p. 173-183
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