Zobrazeno 1 - 10
of 362
pro vyhledávání: '"T. Adatte"'
Autor:
N. Sharma, J. E. Spangenberg, T. Adatte, T. Vennemann, L. Kocsis, J. Vérité, L. Valero, S. Castelltort
Publikováno v:
Climate of the Past, Vol 20, Pp 935-949 (2024)
The Middle Eocene Climatic Optimum (MECO) is a global warming event mainly recognized in the marine domain and described less in the terrestrial environment. Here we present a comprehensive geochemical record of the MECO from the Escanilla Formation,
Externí odkaz:
https://doaj.org/article/720f0d214f584120a94249b6e10535a7
Autor:
M. T. Jones, E. W. Stokke, A. D. Rooney, J. Frieling, P. A. E. Pogge von Strandmann, D. J. Wilson, H. H. Svensen, S. Planke, T. Adatte, N. Thibault, M. L. Vickers, T. A. Mather, C. Tegner, V. Zuchuat, B. P. Schultz
Publikováno v:
Climate of the Past, Vol 19, Pp 1623-1652 (2023)
There is a temporal correlation between the peak activity of the North Atlantic Igneous Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the NAIP may have initiated and/or prolonged this extreme warming event. Howeve
Externí odkaz:
https://doaj.org/article/61c7f021a6324eb79981507baefaf9df
Autor:
S. Peris Cabré, L. Valero, J. E. Spangenberg, A. Vinyoles, J. Verité, T. Adatte, M. Tremblin, S. Watkins, N. Sharma, M. Garcés, C. Puigdefàbregas, S. Castelltort
Publikováno v:
Climate of the Past, Vol 19, Pp 533-554 (2023)
The early Cenozoic marine sedimentary record is punctuated by several brief episodes ( kyr) of abrupt global warming, called hyperthermals, that have disturbed ocean life and water physicochemistry. Moreover, recent studies of fluvial–deltaic syste
Externí odkaz:
https://doaj.org/article/9edfd5ee2bc648b89f2076d896b30318
Autor:
R. Fentimen, E. Feenstra, A. Rüggeberg, E. Hall, V. Rime, T. Vennemann, I. Hajdas, A. Rosso, D. Van Rooij, T. Adatte, H. Vogel, N. Frank, A. Foubert
Publikováno v:
Climate of the Past, Vol 18, Pp 1915-1945 (2022)
This study provides a detailed reconstruction of cold-water coral mound build-up within the East Melilla Coral Province (southeastern Alboran Sea), more precisely at the northern part of Brittlestar Ridge I, over the last 300 kyr. The multiproxy inve
Externí odkaz:
https://doaj.org/article/282fac2715de48a0b57bf2a6c15e1512
Autor:
M. Moustapha, L. Deirmendjian, D. Sebag, J.-J. Braun, S. Audry, H. Ateba Bessa, T. Adatte, C. Causserand, I. Adamou, B. Ngounou Ngatcha, F. Guérin
Publikováno v:
Biogeosciences, Vol 19, Pp 137-163 (2022)
Tropical rivers emit large amounts of carbon dioxide (CO2) to the atmosphere, in particular due to large wetland-to-river carbon (C) inputs. Yet, tropical African rivers remain largely understudied, and little is known about the partitioning of C sou
Externí odkaz:
https://doaj.org/article/b3bc114c50f944cfb6c3fa8639904919
Publikováno v:
Solid Earth, Vol 11, Pp 2463-2485 (2020)
Some 20 Myr after the Late Jurassic to Early Cretaceous obduction and collision at the eastern margin of Adria, the eroded Pelagonia (Adria)–Axios/Vardar (oceanic complex) contact collapsed, forming the Kallipetra Basin, described around the Aliakm
Externí odkaz:
https://doaj.org/article/dd00ce25a4ed452980ef192663d1c7af
Alluvial record of an early Eocene hyperthermal within the Castissent Formation, the Pyrenees, Spain
Autor:
L. Honegger, T. Adatte, J. E. Spangenberg, J. K. C. Rugenstein, M. Poyatos-Moré, C. Puigdefàbregas, E. Chanvry, J. Clark, A. Fildani, E. Verrechia, K. Kouzmanov, M. Harlaux, S. Castelltort
Publikováno v:
Climate of the Past, Vol 16, Pp 227-243 (2020)
The late Palaeocene to the middle Eocene (57.5 to 46.5 Ma) recorded a total of 39 hyperthermals – periods of rapid global warming documented by prominent negative carbon isotope excursions (CIEs) as well as peaks in iron content – have been rec
Externí odkaz:
https://doaj.org/article/4f527b96d72d4d3797555c75739b0f9b
Autor:
K. B. Föllmi, M. Bôle, N. Jammet, P. Froidevaux, A. Godet, S. Bodin, T. Adatte, V. Matera, D. Fleitmann, J. E. Spangenberg
Publikováno v:
Climate of the Past, Vol 8, Iss 1, Pp 171-189 (2012)
A detailed geochemical analysis was performed on the upper part of the Maiolica Formation in the Breggia (southern Switzerland) and Capriolo sections (northern Italy). The analysed sediments consist of well-bedded, partly siliceous, pelagic carbonate
Externí odkaz:
https://doaj.org/article/7a53549bd7ec4e799541968132fed90e
Autor:
M. Hernández, A. Arciniega-Ceballos, T. Adatte, E. Escobar-Hernández, H.-W. Hubberten, J. Werner, M.A. Ruiz-Martínez, J. Urrutia-Fucugauchi, A. De León
Publikováno v:
Geofísica Internacional, Vol 42, Iss 1, Pp 25-39 (2003)
We report initial results of an interdisciplinary study of the lacustrine sequence of Laguna de Santa Rosa, based on a 26 m long core recovered from its northern-central sector. The Laguna is an intramontane elongated basin with a small catchment are
Externí odkaz:
https://doaj.org/article/9df72ed07f65438890618ed2ac0d1e99
Autor:
J. Urrutia-Fucugauchi, M. A. Ruiz-Martínez, J. Werner, H. W. Hubberten, T. Adatte, E. Escobar-Hernández, A. Arciniega-Ceballos, M. Hernández, A. De León
Publikováno v:
Geofísica Internacional, Vol 42, Iss 1, Pp 25-39 (2003)
Se reportan resultados iniciales del estudio interdisciplinario de la secuencia lacustre de Laguna Santa Rosa, en el núcleo de 26 m de longitud recuperado en el sector norte-centro. Santa Rosa es una cuenca intermontaña, con una reducida zona de ca
Externí odkaz:
https://doaj.org/article/37713405c1f44e5ba61c314f81958835