Sharks ( Neoselachii) and palynomorphs from Mendoza ( Argentina): new evidence of the Late Cretaceous Atlantic marine transgression

被引:10
作者
Pramparo, Mercedes B. [1 ]
Cione, Alberto L. [2 ]
Gonzalez Riga, Bernardo [3 ,4 ]
机构
[1] IANIGLA CONICET, CCT Mendoza, RA-5500 Mendoza, Argentina
[2] Museo La Plata, Div Paleontol Vertebrados, RA-1900 La Plata, Buenos Aires, Argentina
[3] IANIGLA CONICET, CCT, RA-5500 Mendoza, Argentina
[4] Univ Nacl Cuyo, ICB, RA-5500 Mendoza, Argentina
来源
ALCHERINGA | 2014年 / 38卷 / 02期
关键词
Neoselachii; shark teeth; Prasinophytes; organic matter assemblages; Late Cretaceous; southern Mendoza; Argentina; NEUQUEN BASIN; NORTHERN PATAGONIA; PALYNOFACIES; BOLIVIA; CHONDRICHTHYANS; ENVIRONMENTS; VERTEBRATES; EVOLUTION; CHARENTES; PALEOGENE;
D O I
10.1080/03115518.2014.849027
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Pramparo, M.B., Cione, A.L. & Gonzalez Riga, B., 2013. Sharks (Neoselachii) and palynomorphs from Mendoza (Argentina): new evidence of the Late Cretaceous Atlantic marine transgression. Alcheringa 38, 000-000. ISSN 0311-5518.Neoselachian (modern shark) teeth and palynomorphs have been recovered from the Late Cretaceous Jaguel Formation in the Province of Mendoza, Argentina. The fossiliferous beds were deposited during the Atlantic transgression that covered northern Patagonia and other parts of South America from the Maastrichtian to the Danian. Teeth of several lamniform sharks are attributed to the anacoracid Squalicorax pristodontus and cf. Serratolamna serrata of indeterminate familial affinity. These taxa became extinct at the end of the Cretaceous and confirm the late Maastrichtian age previously assigned to the Jaguel Formation in this northwestern part of the Neuquen Basin. For the first time, the selachian faunas are described together with algae and dispersed organic matter assemblages (palynofacies), revealing new elements of the neritic biota leading up to the Cretaceous-Paleogene (K-Pg) mass extinction in South America. The palynoflora consists exclusively of the prasinophyte algae Tasmanites, Cymatiosphaera and Pterospermella, indicative of stratified saline waters. Dispersed organic components in the profile (mainly opaque equidimensional phytoclasts and prasinophytes) are consistent with an inner neritic environment, with evidence (a great variety of particle sizes, lath-shaped phytoclasts increasing slightly in number and decreasing number of marine components) of slightly more nearshore conditions towards the upper part of the profile. These marine biotas confirm the presence of an epeiric sea over northern Patagonia, which extended westwards to the volcanic arc on the western flank of the Andean Cordillera in Mendoza.Mercedes B. Pramparo [mprampar@mendoza-conicet.gov.ar], IANIGLA-CONICET, CCT-Mendoza. Avda. R. Leal s/n, Parque Gral. San Martin, (5500) Mendoza, Argentina; Alberto Luis Cione [acione@museo.fcnym.unlp.edu.ar], Division Paleontologia de Vertebrados. Museo de La Plata. 1900 La Plata, Argentina; Bernardo Gonzalez Riga [bgonriga@mendoza-conicet.gov.ar] IANIGLA-CONICET, CCT, Mendoza. Avda. R. Leal s/n, Parque Gral. San Martin, (5500) and ICB, Universidad Nacional de Cuyo, Argentina. Received 28.5.2013, revised 17.9.2013, accepted 24.9.2013. ????Neoselachian ???????????Mendoza?????Jaguel??????????????????????Maastrichtian??Danian?????Patagonia????????????lamniform???????anacoracid Squalicorax pristodontus?cf. Serratolamna serrate, ?????????????????????, ?????Maastrichtian???, ???????Neuquen??????Jaguel???????selachian????????????????(???)????? , ??????? - ????(K -PG)?????????????????????????prasinophyte??Tasmanites , Cymatiosphaera?Pterospermella ??, ??????????????????(??????????????)?????????, ?????????(??????, ???????????????????????)???????????????????Patagonia????????, ??????Mendoza???????????
引用
收藏
页码:177 / 189
页数:13
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