AFRICAN LEGUME AFFINITIES WITH THE FLORA FROM THE LOWER LA PLATA BASIN (UPPER CENOZOIC), SOUTH AMERICA

被引:1
|
作者
Moya, Eliana [1 ,2 ]
Ramos, R. Soledad [1 ,3 ]
Franco, M. Jimena [1 ,3 ]
Brea, Mariana [1 ,3 ,4 ]
机构
[1] Univ Autonoma Entre Rios UADER, Fac Ciencia & Tecnol, Lab Biol, Sede Diamante, Tratado Pilar 314,E3105AUD, Diamante, Entre Rios, Argentina
[2] Consejo Nacl Invest Cient & Tecn CONICET, Buenos Aires, DF, Argentina
[3] Ctr Invest Cient & Transferencia Tecnol Prod CICY, Lab Paleobot, Espana 149,E3105BWA, Diamante, Entre Rios, Argentina
[4] Univ Nacl La Plata UNLP, Fac Ciencias Nat & Museo, Catedra Paleobot, Calle 122 & 60 S-N, RA-1900 La Plata, Buenos Aires, Argentina
关键词
Fossil woods; Paleophytogeography; Tropical African flora; Neotropical flora; Caesalpinioideae; Detarioideae; FORMATION LATE PLEISTOCENE; TRIBE CAESALPINIEAE LEGUMINOSAE; SP-NOV FABACEAE; WOOD ANATOMY; FOSSIL WOOD; ENTRE RIOS; SUBFAMILY DETARIOIDEAE; ITUZAINGO FORMATION; DOMINICAN AMBER; NORTH-AMERICA;
D O I
10.5710/AMGH.25.08.2022.3521
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
This article presents an analysis of the affinities of legumes from the upper Cenozoic of the lower La Plata Basin (South America) with extant African genera and their implications for paleoecology and paleophytogeography. Permineralized woods, assigned to Entrerrioxylon victoriensis from the Parana Formation (upper Miocene), Gossweilerodendroxylon palmariensis and Paraoxystigma concordiensis from the El Palmar Formation (upper Pleistocene), and Cylicodiscuxylon paragabunensis from the Arroyo Feliciano Formation (upper Pleistocene), show affinities with extant genera of the Detarioideae and Caesalpinioideae (mimosoid clade). Today, the taxa of the Detarioideae are distributed mainly in tropical regions of Africa, Central America and South America, and the monotypic genus Cylicodiscus is restricted to West Africa from Sierra Leone to Gabon. Currently, Cylicodiscus, Gossweilerodendron, and Oxystigma are not distributed in South America, which implies that in the past they were widely distributed and became extinct in this region at some point during the Pleistocene-Holocene, presumably related to the climatic changes that occurred during this time. The fossil record of the lower La Plata Basin with taxa related to the Detarioideae and Cylicodiscus supports a wider distribution during the Cenozoic as well as an ancient relationship with the tropical forests of West Africa.
引用
收藏
页码:48 / 64
页数:17
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