New palynological record for the Puesto Albornoz Formation (Golfo San Jorge basin, Argentina): Stratigraphic and paleoenvironmental implications

被引:1
|
作者
Loinaze, Valeria S. Perez [1 ,5 ]
Llorens, Magdalena [2 ,3 ,5 ]
Rodriguez, Agustin R. [4 ,5 ]
Allard, Jose O. [4 ]
Foix, Nicolas [1 ,4 ,5 ]
机构
[1] Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat Bernardino Rivadavia, Ave Angel Gallardo 470 C1405DJR, Buenos Aires, Argentina
[2] Univ Nacl La Patagonia San Juan Bosco, Lab Bot, 9 Julio 25 U9100CKN, Trelew, Argentina
[3] Univ Nacl La Patagonia San Juan Bosco, Fac Ciencias Nat & Ciencias Salud, Lab Palinol, 9 Julio 25 U9100CKN, Trelew, Argentina
[4] Univ Nacl La Patagonia San Juan Bosco UNPSJB, Fac Ciencias Nat & Ciencias Salud, Dept Geol, Ruta Prov N 1 S-N Km4 9005, RA-9005 Comodoro Rivadavia, Argentina
[5] Consejo Nacl Invest Cient & Tecn CONICET, Comodoro Rivadavia, Argentina
关键词
MEMBER AGRIO FORMATION; CRUZ PROVINCE; NEUQUEN BASIN; AUSTRAL BASIN; PATAGONIA; POLLEN; SECTION; CHEIROLEPIDIACEAE; PALYNOFACIES; PALYNOMORPHS;
D O I
10.1016/j.jsames.2024.104804
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Palynomorph assemblages were recovered from the Puesto Albornoz Formation (Golfo San Jorge Basin, Southern Argentina) at its type locality. The scarcity of outcrops with a continental Lower Cretaceous sedimentary record in this basin, and its marginal position in the western sector of the studied area, make Puesto Albornoz a unique and key locality for determining the timing of the basin evolution during the Cretaceous. The palynological content includes thirty-five spore species, twenty-one pollen taxa, and two algae. Among the fifty-eight species identified, forty-eight were identified for the first time for the unit. Based on the previous records of the analyzed taxa, a late Valanginian to Barremian, and more probably late Valanginian to Hauterivian age is inferred for the studied palynoflora. The palynological assemblages studied here closely resemble the Interulobites-Foraminisporis Zone (late Valangian-Hauterivian) of the Argentinian Patagonia, and the Cyclusphaera psilata-Classopollis association (late Valanginian-Barremian) of the Neuque ' n Basin.
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页数:12
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