2022
DOI: 10.1016/j.palaeo.2022.111044
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Changes in benthic microfossil assemblages before, during and after the early Toarcian biotic crisis in the Portland-Wight Basin (Kerr McGee 97/12-1 well, offshore southern England)

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Cited by 11 publications
(2 citation statements)
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“…The ostracod assemblages determined for the stratigraphic interval of the Cenomanian-Turonian transition indicate the presence of a biological event corresponding to the explosion of smooth ostracods called the Cytherellid Event, also described in Spain (Barroso-Barcenilla et al, 2011), Egypt (Shahin & Elbaz, 2013a) and Algeria (Benadla et al, 2018). Cytherellids are relatively resistant to oxygen depleted conditions (Whatley, 1991(Whatley, , 1995 and Cytherella has been interpreted as an ostracod indicative of warm waters adapted to survive during low oxygen episodes (Depêche, 1984;Whatley, 1995;Bonnet et al, 1999;N'Zaba-Makaya et al, 2003;Reolid, 2020;Reolid & Ainsworth, 2022). In the Rhoundjala section the Cytherellid Event coincides with the negative carbon isotopic excursion of the OAE2 (Benadla et al, 2018).…”
Section: Interpretation and Comparison With Other Regionsmentioning
confidence: 99%
“…The ostracod assemblages determined for the stratigraphic interval of the Cenomanian-Turonian transition indicate the presence of a biological event corresponding to the explosion of smooth ostracods called the Cytherellid Event, also described in Spain (Barroso-Barcenilla et al, 2011), Egypt (Shahin & Elbaz, 2013a) and Algeria (Benadla et al, 2018). Cytherellids are relatively resistant to oxygen depleted conditions (Whatley, 1991(Whatley, , 1995 and Cytherella has been interpreted as an ostracod indicative of warm waters adapted to survive during low oxygen episodes (Depêche, 1984;Whatley, 1995;Bonnet et al, 1999;N'Zaba-Makaya et al, 2003;Reolid, 2020;Reolid & Ainsworth, 2022). In the Rhoundjala section the Cytherellid Event coincides with the negative carbon isotopic excursion of the OAE2 (Benadla et al, 2018).…”
Section: Interpretation and Comparison With Other Regionsmentioning
confidence: 99%
“…Other processes documented during the Jenkyns Event include: (1) a perturbation of the carbon cycle evidenced as a negative carbon isotopic excursion (CIE; e.g., Jenkyns & Clayton, 1986;Kemp et al, 2005;Hesselbo et al, 2007;Ruebsam et al, 2019Ruebsam et al, , 2020a; (2) oxygen depleted conditions in some marine basins, the Toarcian Oceanic Anoxic Event (T-OAE, Gill et al, 2011;Fonseca et al, 2018;Izumi et al, 2018;Ruebsam et al, 2018;Suan et al, 2018); (3) a sea-level rise (e.g., Hallam, 1981;Pittet et al, 2014;Haq, 2018;Krencker et al, 2019); and (4) a crisis of marine carbonate productivity (Bucefalo-Palliani et al, 2002;Mattioli et al, 2004) and acidification (Müller et al, 2020;Ettinger et al, 2021). In the context of environmental change, the early Toarcian is also characterized by a second-order extinction that affected marine ecosystems, including dynoflagellate cysts, foraminifera, ostracods, brachiopods, corals, bivalves, and cephalopods (e.g., Hallam, 1987;Little & Benton, 1995;Harries & Little, 1999;Aberhan & Fürsich, 2000;Macchioni & Cecca, 2002;Vörös, 2002;Arias, 2009Arias, , 2013Dera et al, 2010;García Joral et al, 2011;Caruthers et al, 2014;Baeza-Carratalá et al, 2017;Reolid et al, 2019;Vasseur et al, 2021;Reolid & Ainsworth, 2022). In addition to the extinction, the biotic crisis is also expressed in a decrease of diversity, mainly affecting benthic communities, as well reductions in body siz...…”
Section: Introductionmentioning
confidence: 99%