Thermal and depositional history of Early-Permian Rio Bonito Formation of southern Paraná Basin – Brazil

Bicca, Marcos Müller; Kalkreuth, W.; Silva, Taís Freitas da; Oliveira, Christie Helouise Engelmann de; Genezini, Frederico A.

doi:10.1016/j.coal.2020.103554

Cited by 11 publications

(3 citation statements)

References 49 publications

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“…Even where radiogenic isotopic dates are available, these have not always provided consistent age constraints on fossiliferous rock units. For example, dating of tuffs from the Rio Bonito Formation of Brazil has yielded ages ranging from Asselian to Roadian (Matos et al, 2001;Cagliari et al, 2014;Griffis et al, 2018;Rocha-Campos et al, 2019), although following Bicca et al (2020), and on palaeobotanical grounds, we would argue that the unit is predominantly of late Sakmarian to Artinskian age. For these reasons, quantitative evaluation of the herbivory records on a Gondwana-wide scale is greatly constrained.…”

Section: Methodsmentioning

confidence: 89%

Arthropod interactions with the Permian Glossopteris flora

McLoughlin

Prevec

Slater

2021

JPS

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An extensive survey of literature on the Permian floras of Gondwana reveals over 500 discrete arthropod–herbivory– damage/plant–taxon/stratigraphic–unit associations spanning all regions of the supercontinent from the earliest Asselian to the latest Changhsingian. Margin– and apex–feeding damage is the most common style of herbivory but hole– and surface–feeding, galling, and oviposition damage are locally well represented. Evidence for skeletonization and mucivory is sparse and that for leaf mining is equivocal. Wood and root boring is recognized widely but only where depositional conditions were conducive to the permineralization of plant axes. Wood boring and detritivory may have been especially favoured arthropod feeding strategies in Permian high latitudes where living foliage was scarce during the polar winters. Herbivory damage is most strongly apparent on glossopterid remains; other groups of broad–leafed gymnosperms and sphenopsids host moderate levels of damage. Damage features are under–represented on lycophytes, ferns and spine– and scale–leafed conifers. A survey of insect body fossils from the Gondwanan Permian reveals that most records are from a small number of rich assemblages that are dominated by Blattodea, Hemiptera, Grylloblattida, Mecoptera and Protelytroptera, accompanied by significant representations of Coleoptera, Glosselytrodea, Miomoptera, Neuroptera, Odonata, Protorthoptera, Palaeodictyopteroida, Paoliida, Paraplecoptera, Plecoptera, Psocoptera, Thysanoptera and Trichoptera, which collectively adopted a broad range of feeding styles. Oribatid mites and collembolans appear to have been important components of the wood–boring and detritivorous communities. Although temporal trends in herbivory styles and diversity are difficult to resolve from mostly incidental observations and illustrations of plant damage across Gondwana, the results of this study provide a baseline of qualitative data for future studies that should adopt a quantitative approach to the analysis of herbivory, spanning the shift from icehouse to hothouse conditions through the Permian of the Southern Hemisphere.

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Section: Methodsmentioning

confidence: 89%

Arthropod interactions with the Permian Glossopteris flora

McLoughlin

Prevec

Slater

2021

JPS

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“…Peat beds and coal-bearing sequences could be eroded due to several reasons (e.g., flooding events and mass movements during peat formation or fluvial and marine influence after coalification) (Petersen et al, 1998;Lindsay and Herbert, 2002;Geršlová et al, 2016;Izart et al, 2016;Martínek et al, 2017;Bicca et al, 2020). As a result, coal clasts and/or coal-placers could be observed within the synchronous siliciclastic sediments and marine carbonates of coal seams and in modern marine sediments (Littke et al, 1989;Hower et al, 2001;Pešek and Sýkorová, 2006;Dill et al, 2017Dill et al, , 2021Zhang et al, 2019;Yang et al, 2020).…”

Section: Introductionmentioning

confidence: 99%

Vitrinite reflectances and mineralogy of coal clasts in the Late Carboniferous sequences in the two-deep research wells from the Kozlu coalfield (Zonguldak Basin, NW Türkiye)

Karayi̇ǧi̇t

Oskay

2022

Bull.Min.Res.Exp.

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Fifty-four coal clast samples in the siliciclastic rocks (e.g., sandstone and conglomerate) were collected from cores of two-deep research wells (K20H and K20K) drilled at the Kozlu coalfield in Zonguldak Basin, and for the first time, they were evaluated using mineralogy by XRD and SEM-EDX and random vitrinite reflectance (%Rr) measurements in order to find out their origin and timing. Petrographic observations on polish surfaces show that the coal clasts are either entirely xylitic/vitrinitic particle or coals including a broader range of macerals. The detected minerals in the samples are mostly derived from the parental coal seams and, to lesser extent, precipitated from penetrated pore-water in the cleats/fractures of clasts. The %Rr values of coal clasts in Carboniferous sediments are generally relatively higher than measured in the coal seams due to weak oxidation during transportation. Furthermore, similar mineralogical and maceral compositions between coal clasts and coal seams imply that these clasts were mainly eroded during the peatification and/or early coalification of parental seams and display similar coalification patterns. The close %Rr value of a coal clast sample in the Early Aptian Zonguldak Formation and Carboniferous coal seams could suggest that this coal clast sample is presumably derived from the coal seams eroded during Early Aptian.

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“…With the support of the research fruit, a new field of studying mineral-fission track annealing, using nuclear fission technology, has emerged [9][10][11][12][13][14][15][16]. Furthermore, the random huminite/vitrinite reflectance and apatite fission-track methods could be useful parameters for evaluating the paleotemperature of thermal and geodynamic evolution, and the burial history of coal-bearing sequences [17][18][19][20][21][22][23][24][25][26].…”

Section: Introductionmentioning

confidence: 99%

Tectono-Thermal Events of Coal-Bearing Basin in the Northern North China Craton: Evidence from Zircon–Apatite Fission Tracks and Vitrinite Reflectance

et al. 2022

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In order to further reveal the tectonic activity of the central and northern North China Craton (NCC) since late Paleozoic, the Datong coal-bearing basin was selected as the research object. The tectono-thermal events and uplifting cooling events of the basin were retrieved through zircon and apatite fission tracks and vitrinite reflectance measurements. The research shows that the Datong coal-bearing basin experienced three tectono-thermal events with ages of 245–207 Ma (middle–late Triassic), 179 ± 9 Ma (early Jurassic), and 140 Ma to 78 ± 11 Ma (middle–late Cretaceous), respectively. That just coincides with the lamprophyre activity, Kouquan fault activity, and Zuoyun basaltic andesite magmatic activity which surround the Datong coalfield. The basin also experienced three uplift events with the peak ages of 202 ± 18 Ma (late Triassic), 157 ± 7 Ma (late Jurassic), and 45 ± 3 Ma or 36 ± 3 Ma (middle Eocene), respectively. The Datong Permo-Carboniferous and Jurassic coal vitrinite reflectance proved that the average metamorphism temperature is 104–108 °C, even reaching 163–367 °C. The fission track results showed that the paleotemperature was even higher than 170–250 °C from 117 to 282 Ma and 80–120 °C from 20 to 68 Ma, in the Datong coal-bearing basin. The results show that the deep tectonic activities of the NCC were still active in the Mesozoic and even Cenozoic Paleogene.

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Thermal and depositional history of Early-Permian Rio Bonito Formation of southern Paraná Basin – Brazil

Cited by 11 publications

References 49 publications

Arthropod interactions with the Permian Glossopteris flora

Arthropod interactions with the Permian Glossopteris flora

Vitrinite reflectances and mineralogy of coal clasts in the Late Carboniferous sequences in the two-deep research wells from the Kozlu coalfield (Zonguldak Basin, NW Türkiye)

Tectono-Thermal Events of Coal-Bearing Basin in the Northern North China Craton: Evidence from Zircon–Apatite Fission Tracks and Vitrinite Reflectance

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