Zobrazeno 1 - 10
of 75
pro vyhledávání: '"Jenkyns, HC"'
Autor:
Dickson, AJ, Idiz, E, Porcelli, D, Murphy, MJ, Celestino, R, Jenkyns, HC, Poulton, SW, Hesselbo, SP, Hooker, JN, Ruhl, M, van den Boorn, SHJM
The isotope ratios of redox-sensitive metals in organic-rich rocks are critical tools for quantifying the timing and severity of deoxygenation and nutrient cycling in Earth's past. The resilience of isotopic data to thermal alteration of the host sed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b40f5ef5aa2eea24b4d16c1d7f2092c6
https://ora.ox.ac.uk/objects/uuid:4dfeeee2-ad0a-4def-8092-62bb75fba2b2
https://ora.ox.ac.uk/objects/uuid:4dfeeee2-ad0a-4def-8092-62bb75fba2b2
Publikováno v:
Global and Planetary Change. 215:103887
The early Toarcian, as registered in a variety of sedimentary archives, was characterized by an abrupt negative carbon-isotope excursion (CIE) typically superimposed on a long-term positive trend, and was accompanied by significant climatic and envir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a2ae9c014c2920bbe22988426859eaa
https://doi.org/10.1016/j.gloplacha.2022.103887
https://doi.org/10.1016/j.gloplacha.2022.103887
Autor:
Scaife, JD, Ruhl, M, Dickson, AJ, Mather, TA, Jenkyns, HC, Percival, LME, Hesselbo, P, Cartwright, J, Eldrett, JS, Bergman, SC, Minisini, D
Oceanic Anoxic Event 2 (OAE 2), during the Cenomanian‐Turonian transition (∼94 Ma), was the largest perturbation of the global carbon cycle in the mid‐Cretaceous and can be recognized by a positive carbon‐isotope excursion in sedimentary stra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2ae238ecded8b58c8d496765c6f7786d
https://doi.org/10.1002/2017gc007153
https://doi.org/10.1002/2017gc007153
Autor:
Linnert, C, Robinson, S, Lees, JA, Pérez-Rodríguez, I, Jenkyns, HC, Petrizzo, MR, Arz, JA, Bown, PR, Falzoni, F
The Campanian – Maastrichtian (83–66 Ma) was a period of global climate cooling, featuring significant negative carbon-isotope (δ13C) anomalies, such as the Late Campanian Event (LCE) and the Campanian – Maastrichtian Boundary Event (CMBE). A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::5ac63286fab3537f9bca8e7892dc19d9
https://ora.ox.ac.uk/objects/uuid:c919cd98-085f-4865-9256-fc44722916ed
https://ora.ox.ac.uk/objects/uuid:c919cd98-085f-4865-9256-fc44722916ed
Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major palaeoceanographic phenomenon that took place during an interval of extreme global warmth when large amounts of organic matter entered the marine burial record, probably trig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7b5fd5accb52d18bb855015da166f14a
https://ora.ox.ac.uk/objects/uuid:00ae535f-7a27-4ac1-9918-38e1cc75bc24
https://ora.ox.ac.uk/objects/uuid:00ae535f-7a27-4ac1-9918-38e1cc75bc24