Understanding carbonate factories through palaeoecological and sedimentological signals – Tribute to Luis Pomar.
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- Sedimentology, 2022, v. 69, n. 1, p. 5, doi. 10.1111/sed.12965
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Works matching IS 00370746 AND DT 2022 AND VI 69 AND IP 1
Results: 15
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How do carbonate factories influence carbonate platform morphology? Exploring production−transport interactions with numerical forward modelling.
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- Sedimentology, 2022, v. 69, n. 1, p. 372, doi. 10.1111/sed.12943
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'Isolated base‐of‐slope aprons': An oxymoron for shallow‐marine fan‐shaped, temperate‐water, carbonate bodies along the south‐east Salento escarpment (Pleistocene, Apulia, southern Italy).
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- Sedimentology, 2022, v. 69, n. 1, p. 345, doi. 10.1111/sed.12941
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Seagrass development in terrigenous‐influenced inner ramp settings during the middle Eocene (Urbasa–Andia Plateau, Western Pyrenees, North Spain).
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- Sedimentology, 2022, v. 69, n. 1, p. 301, doi. 10.1111/sed.12937
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Shallow‐marine carbonate cementation in Holocene segments of the calcifying green alga Halimeda.
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- Sedimentology, 2022, v. 69, n. 1, p. 282, doi. 10.1111/sed.12927
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Florida Bay: Modern analogue for Lofer cyclothems?
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- Sedimentology, 2022, v. 69, n. 1, p. 254, doi. 10.1111/sed.12918
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Early Miocene carbonate ramp development in a warm ocean, North West Shelf, Australia.
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- Sedimentology, 2022, v. 69, n. 1, p. 219, doi. 10.1111/sed.12917
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Carbonate tufas as archives of climate and sedimentary dynamic in volcanic settings, examples from Gran Canaria (Spain).
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- Sedimentology, 2022, v. 69, n. 1, p. 199, doi. 10.1111/sed.12908
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9
Issue Information.
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- Sedimentology, 2022, v. 69, n. 1, p. i, doi. 10.1111/sed.12893
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- Article
10
Bryozoan‐rich stromatolites (bryostromatolites) from the Silurian of Gotland and their relation to climate‐related perturbations of the global carbon cycle.
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- Sedimentology, 2022, v. 69, n. 1, p. 162, doi. 10.1111/sed.12863
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11
Response of large benthic foraminifera to climate and local changes: Implications for future carbonate production.
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- Sedimentology, 2022, v. 69, n. 1, p. 121, doi. 10.1111/sed.12858
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Columnar microbialites of the upper Miocene of Mallorca (Spain): A new morphogenetic model based on concurrent accretion and bioturbation – uncommon or overlooked?
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- Sedimentology, 2022, v. 69, n. 1, p. 88, doi. 10.1111/sed.12850
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13
Why did some larger benthic foraminifera become so large and flat?
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- Sedimentology, 2022, v. 69, n. 1, p. 74, doi. 10.1111/sed.12837
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14
The mantle, CO<sub>2</sub> and the giant Aptian chemogenic lacustrine carbonate factory of the South Atlantic: Some carbonates are made, not born.
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- Sedimentology, 2022, v. 69, n. 1, p. 47, doi. 10.1111/sed.12835
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MECO and Alpine orogenesis: Constraints for facies evolution of the Bartonian nummulitic and Solenomeris limestone in the Argentina Valley (Ligurian Alps).
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- Sedimentology, 2022, v. 69, n. 1, p. 24, doi. 10.1111/sed.12829
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