共 42 条
SYSTEMATICS, TAPHONOMY, AND PALEOECOLOGY OF HOMALONOTID TRILOBITES (PHACOPIDA) FROM THE PONTA GROSSA FORMATION (DEVONIAN), PARANA BASIN, BRAZIL
被引:16
|作者:
Simoes, Marcello Guimaraes
[1
]
Leme, Juliana De Moraes
[2
]
Soares, Sabrina Pereira
机构:
[1] UNESP, Dept Zool, BR-18618000 Botucatu, SP, Brazil
[2] Univ Sao Paulo, Dept Geol Sedimentar & Ambiental, IGc, BR-05508080 Sao Paulo, Brazil
来源:
REVISTA BRASILEIRA DE PALEONTOLOGIA
|
2009年
/
12卷
/
01期
基金:
巴西圣保罗研究基金会;
关键词:
Homalonotidae;
Systematics;
Devonian;
Ponta Grossa Formation;
Parana Basin;
D O I:
10.4072/rbp.2009.1.03
中图分类号:
Q91 [古生物学];
学科分类号:
0709 ;
070903 ;
摘要:
Homalonotid trilobites (Phacopida) from the Ponta Grossa Formation (Lower Devonian), Parana State are revised. A total of 156 specimens recovered from rocks that belong to the Jaguariaiva Member (or Sequence B), of the Ponta Grossa Formation cropping out at Ponta Grossa, Tibagi and Jaguariaiva counties, were examined. Data gathered indicate that at least two species are present (Burmeisteria noticus and B. herscheli). B. noticus is a conspicuous species of the Devonian rocks of South Africa (Bokkeveld Group), Argentina (Lipeon Formation), Bolivia (Icla and Belen Formations), and Brazil (Pimenteiras and Ponta Grossa formations). B. herscheli is common in Devonian strata on the Falkland Islands (Fox Bay Formation), South Africa (Bokkeveld Group), and Bolivia (Icla and Tarija formations). and is a newly recognized member of the trilobite fauna of the Ponta Grossa Formation. Hence, the homalonotid fauna of the Ponta Grossa Formation is not monospecific, as previously assumed. Finally, homalonotids are not randomly distributed throughout the succession of the Ponta Grossa Formation. B. herscheli shows a more restricted bathymetric distribution. preferentially occurring in sandstones and siltstones deposited just at the storm wave base. B. noticus lived and/or were preserved in sedimentary deposits varying from sandy facies, generated just in and/or above the fair weather wave base. and in muddy facies deposited below storm wave base. Despite the differences in the distribution of both species, homalonotid remains are rather abundant in the shallow water facies, deposited jus at or above storm wave base, being potentially important paleoenvironmental (neritic facies) indicators.
引用
收藏
页码:27 / 42
页数:16
相关论文