Ostracods from the Cretaceous-Palaeogene boundary at El Matuasto Section, Neuquén Basin, Argentina: taxonomy, palaeoecological and palaeobiogeographical inferences

被引:0
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作者
Ceolin, Daiane [1 ]
Santos Filho, Marcos Antonio B. [1 ]
Concheyro, Andrea [2 ]
Fauth, Gerson [1 ]
机构
[1] Univ Vale Rio Sinos UNISINOS, Inst Tecnol Paleoceanog & Mudancas Climat Itt Ocea, Ave Unisinos 950, BR-93022750 Sao Leopoldo, RS, Brazil
[2] Univ Buenos Aires, IDEAN Inst Estudios Andinos Don Pablo Groeber, Consejo Nacl Invest Cient & Tecn, Fac Ciencias Exactas & Nat, Pabellon 2,Ciudad Univ, RA-1428 Buenos Aires, Argentina
关键词
marine Ostracoda; Neuquen Basin; Maastrichtian; Danian; palaeoecology; palaeobiogeography; NEUQUEN BASIN; DECCAN VOLCANISM; PLANKTIC FORAMINIFERA; TERTIARY BOUNDARY; MASS EXTINCTION; ASTEROID IMPACT; NORTH-ATLANTIC; PATAGONIA; EVOLUTION; CRUSTACEA;
D O I
10.1002/spp2.1549
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
This work presents a taxonomic, palaeoecological and palaeobiogeographical study of the ostracod fauna around the Cretaceous-Palaeogene boundary from the El Matuasto section, Neuquen Basin, Argentina. The analysis of 64 samples resulted in the recovery of 82 marine ostracod species, of which four are new: Hemiparacytheridea condilomata, Paramunseyella stictus, Hysterocythereis acuminata and Aleisocythereis? picnus. In addition, the genera Sapucariella, Monoceratina, Aracajuia, Microceratina and Pelecocythere are reported for the first time from the Neuquen Basin. Palaeoecological inferences indicate fluctuations in abundance and diversity, occurring alongside environmental change from an inner to medium shelf during the Maastrichtian and to an outer shelf in the Danian. The Maastrichtian fauna was less abundant than that in the Danian, which shows a rapid recovery after the Cretaceous-Palaeogene boundary. During the Danian, a small interval also shows a sudden decrease in abundance and diversity that could potentially be related to the Dan-C2 event. In addition, the described genera and species in this study suggest a strong palaeobiogeographical affinity with the Paraiba Basin, northeastern Brazil.
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