Hierarchy of tectonic control on stratigraphic signatures: Base-level changes during the Early Permian in the Paraná Basin, southernmost Brazil

Holz, Michael; Küchle, Juliano; Philipp, Ruy Paulo; Bischoff, Alan; Arima, Naoki

doi:10.1016/j.jsames.2006.09.007

Cited by 64 publications

(48 citation statements)

References 18 publications

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“…Otherwise, detailed sequence stratigraphy analyses carried out by Holz (1999) and Holz et al (2000Holz et al ( , 2006 on this stratigraphic interval on the study area, indicate an unconformity, marking a base-level fall, also recorded at other locations (Alves and Ade, 1996;Holz, 1997). The truncation of the stratigraphic range of the P. goraiensis Subzone due to that unconformity complicates its temporal significance.…”

Section: Stratigraphic Implicationsmentioning

confidence: 61%

Radiometric age determination of tonsteins and stratigraphic constraints for the Lower Permian coal succession in southern Paraná Basin, Brazil

Guerra-Sommer

Cazzulo-Klepzig

Santos

et al. 2008

International Journal of Coal Geology

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Section: Stratigraphic Implicationsmentioning

confidence: 61%

Radiometric age determination of tonsteins and stratigraphic constraints for the Lower Permian coal succession in southern Paraná Basin, Brazil

Guerra-Sommer

Cazzulo-Klepzig

Santos

et al. 2008

International Journal of Coal Geology

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“…Hence, the geotectonic framework of the basement is characterized by several cratonic blocks and intervening mobile belts, forming a complex framework of lineaments and crustal discontinuities which influenced sedimentation due to differential subsidence and uplift of the tectonic blocks (Holz et al, 2006).…”

Section: Introductionmentioning

confidence: 99%

A stratigraphic chart of the Late Carboniferous/Permian succession of the eastern border of the Paraná Basin, Brazil, South America

Holz

França²,

Souza

et al. 2010

Journal of South American Earth Sciences

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320

230

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“…Hence, the geotectonic framework of the basement is characterized by several cratonic blocks and intervening mobile belts, forming a complex framework of lineaments and crustal discontinuities that influenced sedimentation patterns due to differential subsidence and uplift of the tectonic blocks (Holz et al 2006).…”

Section: Geological Settingmentioning

confidence: 99%

Early Devonian (Late Emsian) shark fin remains (Chondrichthyes) from the Paraná Basin, southern Brazil

Richter

Bosetti

Horodyski

2017

An. Acad. Bras. Ciênc.

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We report on the pioneering discovery of Devonian fish remains in the Paraná Basin, which represents the southernmost record of fishes from that period in mainland South America. The material comes from an outcrop at the lower portion of the São Domingos Formation, within Sequence C of the Paraná-Apucarana sub-basin in Tibagi, State of Paraná. Marine invertebrates are abundant in the same strata. The dark colored fish remains were collected in situ and represent natural moulds of partially articulated shark fin rays (radials). No elements such as teeth or prismatic cartilage have been preserved with the fins rays. This can be attributed to the dissolution of calcium-phosphatic minerals at the early stages of fossilization due to diagenetic processes possibly linked to strong negative taphonomic bias. This may have contributed to the fact that fishes remained elusive in the Devonian strata of this basin, despite substantial geological work done in the Paraná State in recent decades. In addition, the scarcity of fish fossils may be explained by the fact that the Devonian rock deposits in this basin originated in a vertebrate impoverished, cold marine environment of the Malvinokaffric Realm, as previously suspected.

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Hierarchy of tectonic control on stratigraphic signatures: Base-level changes during the Early Permian in the Paraná Basin, southernmost Brazil

Cited by 64 publications

References 18 publications

Radiometric age determination of tonsteins and stratigraphic constraints for the Lower Permian coal succession in southern Paraná Basin, Brazil

Radiometric age determination of tonsteins and stratigraphic constraints for the Lower Permian coal succession in southern Paraná Basin, Brazil

A stratigraphic chart of the Late Carboniferous/Permian succession of the eastern border of the Paraná Basin, Brazil, South America

Early Devonian (Late Emsian) shark fin remains (Chondrichthyes) from the Paraná Basin, southern Brazil

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