The fossil genus Aextoxicoxylon (Magnoliopsida) in the Upper Cretaceous Puntudo Chico Formation, Chubut Province, Argentina

被引:11
作者
Ignacio Vera, Ezequiel [1 ,2 ,6 ]
Perez Loinaze, Valeria S. [1 ,6 ]
Llorens, Magdalena [3 ,4 ,6 ]
Gabriel Passalia, Mauro [5 ,6 ]
机构
[1] Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat Bernardino Rivadavia, Av Angel Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina
[2] Univ Buenos Aires, Area Paleontol, Dept Geol, Pabellon 2,Ciudad Univ,C1428EGA, Buenos Aires, DF, Argentina
[3] Univ Nacl La Patagonia San Juan Bosco, Fac Ciencias Nat, Lab Bot, 9 Julio 25,U9100CKN, Trelew, Chubut, Argentina
[4] Univ Nacl La Patagonia San Juan Bosco, Fac Ciencias Nat, Lab Palinol, 9 Julio 25,U9100CKN, Trelew, Chubut, Argentina
[5] CONICET UNCo, INIBIOMA, Av Pioneros 2350, RA-8400 San Carlos De Bariloche, Rio Negro, Argentina
[6] Consejo Nacl Invest Cient & Tecn CONICET, Buenos Aires, DF, Argentina
关键词
Dicotyledonous wood; Maastrichtian; Campanian; Patagonia; Kawas Sea; Angiosperm; WOOD ANATOMY; LIVINGSTON ISLAND; ANTARCTICA; PATAGONIA; 1ST; PALEOENVIRONMENTS; PALEOECOLOGY; DILLENIACEAE; AFFINITIES; EVOLUTION;
D O I
10.1016/j.cretres.2019.104315
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A new fossil dicot wood recovered from the Upper Cretaceous Puntudo Chico Formation is here identified as a representative of the fossil genus Aextoxicoxylon. Differences with the type species support the recognition of a new species, Aextoxicoxylon kawasianus sp. nov. This new taxon is characterized by having indistinct growth rings, solitary vessels, diffuse porosity, perforation plates scalariform with high number of bars, and heterocellular rays. All these features are typical of primitive woods according to Baileyan trends. Furthermore, anatomy of the wood, and the presence of fungal hyphae in vessels, suggests non-seasonal and probably warm and humid climate, which agrees with previous proposals for the Puntudo Chico Formation and other units of similar ages. Aextoxicoxylon is a new element previously not recognized in the Late Cretaceous to Danian floristic assemblages that seem to have been linked to the Kawas Sea, a shallow sea that developed in Patagonia at the end of the Cretaceous. (C) 2019 Elsevier Ltd. All rights reserved.
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页数:8
相关论文
共 61 条
[1]   Malargue Group (Maastrichtian-Danian) deposits in the Neuquen Andes, Argentina: Implications for the onset of the first Atlantic transgression related to Western Gondwana break-up [J].
Aguirre-Urreta, B. ;
Tunik, M. ;
Naipauer, M. ;
Pazos, P. ;
Ottone, E. ;
Fanning, M. ;
Ramos, V. A. .
GONDWANA RESEARCH, 2011, 19 (02) :482-494
[2]  
Anselmi G., 2004, I GEOLOGIA RECURSOS, V31, P1
[3]   THE AGE AND DIVERSIFICATION OF THE ANGIOSPERMS RE-REVISITED [J].
Bell, Charles D. ;
Soltis, Douglas E. ;
Soltis, Pamela S. .
AMERICAN JOURNAL OF BOTANY, 2010, 97 (08) :1296-1303
[4]   Is porous wood structure exclusive of deciduous trees? [J].
Boura, Anais ;
De Franceschi, Dario .
COMPTES RENDUS PALEVOL, 2007, 6 (6-7) :385-391
[5]   Paleoecology and paleoenvironments of Podocarp trees in the Ameghino Petrified forest (Golfo San Jorge Basin, Patagonia, Argentina): Constraints for Early Paleogene paleoclimate [J].
Brea, M. ;
Matheos, S. D. ;
Raigemborn, M. S. ;
Iglesias, A. ;
Zucol, A. F. ;
Pramparo, M. .
GEOLOGICA ACTA, 2011, 9 (01) :13-28
[7]  
Carlquist S, 2003, SYST BOT, V28, P317
[8]  
CARLQUIST S, 1984, Aliso, V10, P505
[9]  
Carlquist S., 2001, COMP WOOD ANATOMY, V2nd, P448, DOI DOI 10.1007/978-3-662-04578-7
[10]  
Casamiquela R.M., 1978, Aspectos ecologicos. Ameghiniana, V15, P137