The influence of terrestrial run off on marine biotic communities: An example from a thrust-top carbonate ramp (Upper Pennsylvanian foreland basin, Picos de Europa, NW Spain)

Merino-Tomé, Oscar; Bahamonde, Juan R.; Samankassou, Elias; Villa, Elisa

doi:10.1016/j.palaeo.2009.04.002

Cited by 23 publications

(15 citation statements)

References 89 publications

(129 reference statements)

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“…Microfaunal data ( Fig. 2; Kochansky-Devidé 1955Merino-Tomé et al 2009;Sremac 2012) have indicated a very similar age for these Croatian deposits. Table 2 summarises the relative abundances of the 19 fossil species that we have seen in the Carboniferous floras from the Velebit Mts.…”

Section: Biostratigraphymentioning

confidence: 85%

“…Terrestrial plant fossils occur in the middle part of the succession, in deposits that are lithologically and faunally similar to the Auernig or Pramollo Group of Kasimovian-Gzhelian age (= Rauserites Zone sensu Merino-Tomé et al 2009), present in the Austrian, Slovenian and Italian Alps (Fritz & Krainer 2006Ronchi et al 2012). Quartz-rich conglomerates, cross-bedded sandstones and graywackes, and bioturbated fossiliferous shales and sandstones are common in the lower part of the group.…”

Section: Geological Backgroundmentioning

confidence: 99%

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Pennsylvanian fossil flora from the Velebit Mountains and Lika region (SW Croatia)

Cleal¹,

Tenchov²,

Sremac³

et al. 2015

Bull. Geosci.

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Section: Biostratigraphymentioning

confidence: 85%

Section: Geological Backgroundmentioning

confidence: 99%

Pennsylvanian fossil flora from the Velebit Mountains and Lika region (SW Croatia)

Cleal¹,

Tenchov²,

Sremac³

et al. 2015

Bull. Geosci.

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“…Likewise, additional occurrences of auloporids have been identified with references in the literature (Minwegen, 2001;Merino Tomé et al, 2009).…”

Section: Materials Of Study and Methodsmentioning

confidence: 99%

“…Likewise she recognized syringoporoids in the Piedrasluengas limestone as well as Neomultithecopora in the Fuente De section, Cantabria (Spain). The Fuente De section (sensu Minwegen, 2001) was also studied by Martínez-Chacón et al (2001) and Merino-Tomé et al (2009), who identified the genus Neomultithecopora, forming small buildups associated with chaetetids, in Cantabria (Spain). Rodríguez et al (1997) identified some taxa of rugose corals in a section near Ribadesella town, Asturias (Spain), where numerous incrustations of auloporid corals occur on the rugose coral skeletons.…”

Section: Introductionmentioning

confidence: 91%

“…In addition, syringoporoids cited and figured in the Picos de Europa Unit, at Morra de Lechugales section in Cantabria province (Minwegen, 2001;Martínez-Chacón et al, 2001;Merino-Tomé et al, 2009) have been also identified from the bibliography. The specimens sampled in the Cantabrian and tabulae, together with the corallite diameter, lumen diameter, and their relationship (diameter/lumen), which helps in the identification of some genera such as Multithecopora and Sinopora.…”

Section: Introduction To Auloporidamentioning

confidence: 96%

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Carboniferous auloporids from the Iberian Peninsula: palaeocology, diversity, and spatio-temporal distribution

Coronado

2014

Journal of Iberian Geology

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Auloporid corals are common in the Palaeozoic and very frequent in the Carboniferous buildups of the Iberian Peninsula. The aim of this study is to analyze the diversity of these corals through a taxonomical recognition of the species and morphotypes that occur in the Iberian Peninsula. Eighteen sections have been sampled between the Ossa-Morena (Mississippian) and Cantabrian (Pennsylvanian) zones dated as upper Viséan to early Kasimovian. In addition, other localities where auloporids occur and are cited in the literature have been also used for this study. The taxonomical identification has been carried out using the criteria proposed by Tchudinova (1980) with little modifications. Thus, eighteen morphotypes and two species belonging to nine nominal genera have been identified (Multithecopora sp. A-H, Syringopora sp. A-B, Aulopora sp. A-B, Cladochonus sp. A-B, Syringoalcyon sp., Roemeripora sp., Sinopora sp., Mastopora? sp., Multithecopora hontoriense and Neomultithecopora cantabrica). Through a classical microfacies study, the environments where the auloporids lived have been identified, as well as the growth patterns and the features of sedimentation. Finally, a preliminary biostratigraphic range chart for the Carboniferous auloporoids from the Iberian Peninsula has been achieved.. Keywords:Iberia, Ossa-Morena Zone, Cantabrian Zone, Auloporid corals, Carboniferous ResumenLos corales aulopóridos son muy comunes en el Paleozoico y muy frecuentes en las bioconstrucciones del Carbonífero de la Península Ibérica. Con el objetivo de analizar la diversidad de estos corales, se ha llevado a cabo un detallado estudio de los morfotipos y especies de aulopóriodos carboníferos que aparecen en la Península Ibérica. Para ello se han estudiado 18 secciones repartidas entre la Zona de Ossa-Morena (Missisípico,) y la Zona Cantábrica (Pennsylvánico), con edades comprendidas entre el Viseense superior y el Kasimoviense inferior. Así mismo para este estudio se han tenido en cuenta otros aulóporidos ya identificados en trabajos previos. La identificación taxonómica se ha realizado siguiendo los criterios propuestos por Tchudinova (1980) con algunas modificaciones. De esta manera se han identificado dieciocho morfotipos y dos especies que pertenecen a nueve géneros (Multithecopora sp A-H, Syringopora sp A-B, Aulopora sp A-B, Cladochonus sp A-B, Syringoalcyon sp, Roemeripora sp, Sinopora sp, Mastopora? sp, Multithecopora hontoriense and Neomultithecopora cantabrica). Mediante un estudio clásico de las microfacies asociadas a los aulopóridos de la Península Ibérica se han identificado los ambientes y características de crecimiento o depósito. Por último se ha realizado una tabla bioestratigráfica preliminar con los datos de los que se dispone actualmente.

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Synorogenic Basins

Oliveira

Clavijo

Alonso

et al. 2019

Regional Geology Reviews

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The influence of terrestrial run off on marine biotic communities: An example from a thrust-top carbonate ramp (Upper Pennsylvanian foreland basin, Picos de Europa, NW Spain)

Cited by 23 publications

References 89 publications

Pennsylvanian fossil flora from the Velebit Mountains and Lika region (SW Croatia)

Pennsylvanian fossil flora from the Velebit Mountains and Lika region (SW Croatia)

Carboniferous auloporids from the Iberian Peninsula: palaeocology, diversity, and spatio-temporal distribution

Synorogenic Basins

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