In: Facies, 2015, vol. 61, no. 4, p. 1-27
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In: Contributions to Mineralogy and Petrology, 2015, vol. 170, no. 3, p. 1-17
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In: The European Physical Journal Special Topics, 2015, vol. 224, no. 17-18, p. 3119-3140
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In: The Cryosphere, 2020, vol. 14, no. 2, p. 521–538
One of the primary controls upon the melting of the Greenland Ice Sheet (GrIS) is albedo, a measure of how much solar radiation that hits a surface is reflected without being absorbed. Lower-albedo snow and ice surfaces therefore warm more quickly. There is a major difference in the albedo of snow-covered versus bare-ice surfaces, but observations also show that there is substantial spatio-...
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In: Proceedings of the Royal Society B: Biological Sciences, 2019, vol. 286, no. 1911, p. 20191506
We develop a spatially explicit model of diversification based on palaeohabitat to explore the predictions of four major hypotheses potentially explaining the latitudinal diversity gradient (LDG), namely, the ‘time-area’, ‘tropical niche conservatism’, ‘ecological limits’ and ‘evolutionary speed’ hypotheses. We compare simulation outputs to observed diversity gradients in the...
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In: Transport in Porous Media, 2019, vol. 129, no. 1, p. 343–383
Accurate prediction of permeability evolution is essential for forecasting the long-term performance and lifetime of hydrothermal reservoirs, an important goal in the geothermal, ore, and petroleum industries. Erol et al. (Transp Porous Media 120(2):327–358, 2017. https://doi.org/10.1007/s11242-017-0923-z) introduced a general (non-empirical) analytical Kozeny–Carman type equation for...
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In: Microbial Ecology, 2014, vol. 68, no. 3, p. 584-595
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In: International Journal of Earth Sciences, 2014, vol. 103, no. 4, p. 1141-1161
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In: Sedimentology, 2019, vol. 66, no. 2, p. 480–512
Pleistocene fibrous aragonite fabrics, including crusts and spherules, occur in the Danakil Depression (Afar, Ethiopia) following the deposition of two distinctive Middle and Late Pleistocene coralgal reef units and pre‐dating the precipitation of evaporites. Crusts on top of the oldest reef unit (Marine Isotope Stage 7) cover and fill cavities within a red algal framework. The younger...
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In: Eclogae Geologicae Helvetiae, 2005, vol. 98, no. 1, p. 19-49
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