Changes in Coral Skeleton Growth Recorded by Density Band Stratigraphy, Crystalline Structure, and Hiatuses

Autor: Kyle W. Fouke, Jeffrey M. Trop, Mayandi Sivaguru

Publikováno v: Frontiers in Marine Science, Vol 8 (2021)

Next-generation high resolution brightfield microscopy, x-radiography, and microcomputed tomography (microCT) analyses indicate that coral skeleton high density band (HDB) and low density band (LDB) stratigraphic sequences record dynamic changes in c

Externí odkaz: https://doaj.org/article/0694813d9b514b2692339855ab9c4b11

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Significant hiatuses in the terrestrial Late Variscan Central and Western Bohemian basins (Late Pennsylvanian–Early Cisuralian) and their possible tectonic and climatic links

Autor: Martínek Karel, Pešek Jiří, Opluštil Stanislav

Publikováno v: Geologica Carpathica, Vol 68, Iss 3, Pp 269-281 (2017)

Significant changes in the stratigraphy of the Central and Western Bohemian Upper Palaeozoic basins occur during or shortly after hiatuses. The different extent and changes in the depocentres of the Radnice and Nýřany members (Moscovian) in the Plz

Externí odkaz: https://doaj.org/article/93547413ddaf4d76b0ac3a12bc33bbfb

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Long-eccentricity regulated climate control on fluvial incision and aggradation in the Palaeocene of north-eastern Montana (USA)

Autor: Noorbergen, Lars J., Turtu, Antonio, Kuiper, Klaudia F., Kasse, Cornelis, van Ginneken, Sverre, Dekkers, Mark J., Krijgsman, Wout, Abels, Hemmo A., Hilgen, Frederik J., Stratigraphy & paleontology, Paleomagnetism, Stratigraphy and paleontology

Publikováno v: Sedimentology, 67(5), 2529. Wiley Online Library
Sedimentology, 67(5), 2529-2560. Wiley-Blackwell
Noorbergen, L J, Turtu, A, Kuiper, K F, Kasse, C, van Ginneken, S, Dekkers, M J, Krijgsman, W, Abels, H A & Hilgen, F J 2020, ' Long-eccentricity regulated climate control on fluvial incision and aggradation in the Palaeocene of north-eastern Montana (USA) ', Sedimentology, vol. 67, no. 5, pp. 2529-2560 . https://doi.org/10.1111/sed.12710
Sedimentology, 67(5)

Aggradation and fluvial incision controlled by downstream base-level changes at timescales of 10 to 500 kyr is incorporated in classic sequence stratigraphic models. However, upstream climate control on sediment supply and discharge variability cause

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a24726543c34b0194585459c6e028b5d
https://hdl.handle.net/1871.1/2a2866ac-c8ea-4b7c-856b-e172c02a582c