Arid
DOI10.1016/j.palaeo.2017.06.027
A new ichnotaxon classification of large mammaliform trackways from the Lower Cretaceous Botucatu Formation, Parana Basin, Brazil
Buck, Pedro Victor1; Ghilardi, Aline Marcele1; dos Reis Fernandes, Luciana Bueno2; Fernandes, Marcelo Adorna2
通讯作者Buck, Pedro Victor
来源期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN0031-0182
EISSN1872-616X
出版年2017
卷号485页码:377-388
英文摘要

During the Early Cretaceous, a large area in Brazil and other South American countries was covered by an extensive paleoerg field, the Botucatu Desert. The Araraquara County (Sao Paulo State, Brazil) contains some of the most diverse ichnological assemblages in the Botucatu Formation. Mammaliform trace fossils from the Botucatu Formation are of great interest, as they may represent the only record of Lower Cretaceous Mammaliamorpha from Brazil. These trace fossils can be grouped into two distinct classes, based on the dimensions of the footprints. The larger morphotype is described and classified as a new ichnotaxon, Aracoaraichnium leonardii igen. nov. isp. nov., with a discussion of preservational features and paleoecological aspects. This morphotype can be differentiated from Brasilichnium Leonardi, 1981 by digit morphology, with digits Ill and IV being larger and sub-equal in size. The tracks are mesaxonic, unlike Brasilichnium, which is ectaxonic, and the stride is proportionally smaller, suggesting a trackmaker with shorter limbs in relation to body length. Another characteristic that reinforces the new ichnotaxon is the larger size of the footprints of Aracoaraichnium igen. nov. Footprints representing intermediate ontogenetic stages between Brasilichnium and the larger morphotype are not observed, suggesting that the two track types were made by different taxa. Compared with others tetrapod ichnotaxa, the new ichnotaxon is characterized by differences in the number and morphology of the digits, track morphology, the degree of heteropody, and locomotor parameters. Tracks with good preservation quality were likely originally produced in the humid subsurface, below the surficial dry sand layer. Tracks with smaller dimensions, and trackways with the presence or absence of the manus, may be due to variable degrees of impression into subsurface layers, and substrate heterogeneity. The Aracoaraichnium igen. nov. trackmakers probably inhabited areas near the desert, making occasional incursions into desert areas, while Brasilichnium trackmakers may have been mostly nocturnal residents of the desert environment. (C) 2017 Elsevier B.V. All rights reserved.


英文关键词Aracoaraichnium leonardii Tetrapod Footprints Paleodesert Mesozoic Ichnology
类型Article
语种英语
国家Brazil
收录类别SCI-E
WOS记录号WOS:000419747400028
WOS关键词TETRAPOD FOOTPRINTS ; DESERT RODENTS ; PRESERVATION ; ARARAQUARA ; PATTERNS
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS研究方向Physical Geography ; Geology ; Paleontology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/201365
作者单位1.Univ Fed Sao Carlos, Ctr Ciencias Biol & Saude, Programa Pos Grad Ecol & Recursos Nat, Rodovia Washington Luis,Km 235-SP-310, BR-13565905 Sao Carlos, SP, Brazil;
2.Univ Fed Sao Carlos, Dept Ecol & Biol Evolut, Lab Paleoecol & Paleoicnol, Rodovia Washington Luis,Km 235-SP-310, BR-13565905 Sao Carlos, SP, Brazil
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Buck, Pedro Victor,Ghilardi, Aline Marcele,dos Reis Fernandes, Luciana Bueno,et al. A new ichnotaxon classification of large mammaliform trackways from the Lower Cretaceous Botucatu Formation, Parana Basin, Brazil[J],2017,485:377-388.
APA Buck, Pedro Victor,Ghilardi, Aline Marcele,dos Reis Fernandes, Luciana Bueno,&Fernandes, Marcelo Adorna.(2017).A new ichnotaxon classification of large mammaliform trackways from the Lower Cretaceous Botucatu Formation, Parana Basin, Brazil.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,485,377-388.
MLA Buck, Pedro Victor,et al."A new ichnotaxon classification of large mammaliform trackways from the Lower Cretaceous Botucatu Formation, Parana Basin, Brazil".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 485(2017):377-388.
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