Zobrazeno 1 - 10
of 75
pro vyhledávání: '"Stuart A. Robinson"'
Publikováno v:
The Depositional Record, Vol 7, Iss 3, Pp 520-540 (2021)
Abstract Waterlogged, reducing soils in modern and ancient wetlands feature distinctive syndepositional to early diagenetic spherical iron carbonate concretions, known as sphaerosiderites. Sphaerosiderites are thought to record pore water elemental c
Externí odkaz:
https://doaj.org/article/efe7633c06094c54b674ef0cc513aa0a
Publikováno v:
Geochimica et Cosmochimica Acta. 326:273-287
The uraniumisotopic composition(δ238U) of bulk marinecalcium carbonateshas been extensively explored as a promising paleoredox proxy to track the extent of global oceanic anoxia in deep time. Multiple studies have examined whether primary calcium ca
Autor:
Francisco M.W. Tognoli, Stuart A. Robinson, Hugh C. Jenkyns, Leonardo R. Tedeschi, Cecília C. Lana, Maria Rosilene F. Menezes Santos
Publikováno v:
Newsletters on Stratigraphy. 53:333-364
Carbon-isotope ratios derived from organic matter (δ13COM) are presented from Petrobras Well D, onshore Brazil, in the Sergipe-Alagoas Basin. These new data provide a unique view of Aptian palaeoenvironmental history of this low-latitude equatorial
Publikováno v:
Geology. 48:483-487
We present evidence that hydrocarbon source rocks can be preconditioned for primary hydrocarbon migration at an early stage of catagenesis by pore-scale processes linked to silica diagenesis. The evidence comes from a detailed petrographic and geoche
Autor:
Stuart Christopher Robinson
Publikováno v:
Revista Digital Mundo Asia Pacífico. 8:20-41
Este reporte proporciona una discusión y recomendaciones sobre la participación de la industria láctea de Nueva Zelanda en Colombia con el objetivo de reducir la pobreza. El tema es de más relevancia en la perspectiva de la negociación actual en
Autor:
Nicholas A. Curry, Stuart F. Robinson
Publikováno v:
The Catholic Historical Review. 108:225-226
A global warming episode in the Late Cretaceous, the Latest Maastrichtian Warming Event (LMWE), has been commonly linked to both the onset of massive Deccan Trap volcanism and the start of a planktic foraminiferal mass extinction prior to the Cretace
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::30be61db6c519cc0136240a0c6419243
https://doi.org/10.1016/j.cretres.2021.104844
https://doi.org/10.1016/j.cretres.2021.104844
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Sietske J. Batenburg, Serginio R. C. Remmelzwaal, Stuart A. Robinson, Hugh C. Jenkyns, Andrew S. Gale, Lauren K. O'Connor, Ian J. Parkinson
Publikováno v:
O'Connor, L K, Jenkyns, H C, Robinson, S A, Remmelzwaal, S R C, Batenburg, S J, Parkinson, I J & Gale, A S 2020, ' A re-evaluation of the Plenus Cold Event, and the links between CO2, temperature, and seawater chemistry during OAE 2 ', Paleoceanography and Paleoclimatology, vol. 35, no. 4, e2019PA003631 . https://doi.org/10.1029/2019PA003631
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, American Geophysical Union, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
Paleoceanography and Paleoclimatology, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, American Geophysical Union, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
Paleoceanography and Paleoclimatology, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
International audience; The greenhouse world of the mid‐Cretaceous (~94 Ma) was punctuated by an episode of abrupt climatic upheaval: Oceanic Anoxic Event 2 (OAE 2). High‐resolution climate records reveal considerable changes in temperature, carb
Autor:
Ian Jarvis, Tamsin A. Mather, Alex Dickson, Hugh C. Jenkyns, Lineke Woelders, Sietske J. Batenburg, Richard S. Barclay, Lawrence Percival, Micha Ruhl, Stuart A. Robinson, Stephen P. Hesselbo
Publikováno v:
American Journal of Science. 318:799-860
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province (LIP) volcanism, and supports hypotheses of a coincidence between the formation of several LIPs and episodes of mass extinction and major environmental perturba