Josep Magrans - Academia.edu (original) (raw)
Papers by Josep Magrans
Northeast Spain�. �Corales tabulados � � estratigraf�a del Dev�nico �nferior � � del Misis�pico e... more Northeast Spain�. �Corales tabulados � � estratigraf�a del Dev�nico �nferior � � del Misis�pico en las inmediaciones de Barcelona �Cordilleras Costeras Catalanas, nordeste de �spa�a�.] Revista Española de Paleontología, 22 �2�, 175-192. �SSN 0213-6937. �n this paper the content of tabulate corals of the Olorda �Lower Devonian � and �l Papiol �Mississipian � Forma-tions near Barcelona (Catalonian Coastal Ranges, NE Spain) are described for the first time. The Olorda Forma-tion was studied in the Bruguers section, where two new tabulate coral species, Petridictyum casanovai n. sp. and Procteria �Granulidictyum�? gavaensis n. sp., have been collected. The �l Papiol Formation was studied in the �l Papiol and Cánoves sections, and four tabulate coral taxa, Sutherlandia? sp., Smythina humilis �Hinde, 1896�, Palaeacis sp. and Cladochonus sp., have been recognised. �n addition, the succession of the Olorda Formation in Bruguers is described. Lochkovian-lowermost Pragian age is established f...
�n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Missis... more �n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Mississipian� Formations near Barcelona (Catalonian Coastal Ranges, NE Spain) are described for the first time. The Olorda Formation was studied in the Bruguers section, where two new tabulate coral species, Petridictyum casanovai n. sp. and Procteria �Granulidictyum�? gavaensis n. sp., have been collected. The �l Papiol Formation was studied in the �l Papiol and Cánoves sections, and four tabulate coral taxa, Sutherlandia? sp., Smythina humilis �Hinde, 1896�, Palaeacis sp. and Cladochonus sp., have been recognised. �n addition, the succession of the Olorda Formation in Bruguers is described. Lochkovian-lowermost Pragian age is established for the B Member of this formation in Bruguers and this section is correlated with the t��pe section of the formation in Santa Creu d’Olorda. Finall��, it is deduced that the sedimentation of the upper part �B Member� of the Olorda Formation, in Bruguers, an...
Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especia... more Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especiament es fa l'estudi de les restes de Myliobatis aquila i de Pteromylauus bovinus. No hi ha distincio amb les especies actuals.
Spanish Journal of Palaeontology, 2021
Se describe la sucesión estratigráfica del Carbonífero y se definen tres formaciones en varias lo... more Se describe la sucesión estratigráfica del Carbonífero y se definen tres formaciones en varias localidades situadas en el sector septentrional de las Cadenas Costeras Catalanas. Se estudian los braquiópodos de la Formación El Papiol en capas de edad próxima al límite Viseense-Serpukhoviense. Los braquiópodos son relativamente escasos y se encuentran casi exclusivamente como moldes internos o externos, con una conservación incompleta, lo que ha obligado a utilizar nomenclatura abierta. Se han identificado los siguientes taxones: Drahanorhynchus cf. paeckelmanni, Globosochonetes? sp. Parmephrix? cf. aprathensis, Chonetipustula cf. concentrica, Martinia sp., Tomiopsis? sp., Kitakamithyris? sp., Phricodothyris? sp. y Plicotorynifer? sp. Las asociaciones de braquiópodos son comparables a las del Viseense en facies Culm del norte de Europa, especialmente de Alemania. La relación también es grande con algunas formaciones carboníferas de la Cordillera Cantábrica, destacando el elevado númer...
Revista Espanola De Paleontologia, Apr 1, 2011
�n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Missis... more �n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Mississipian� Formations near Barcelona (Catalonian Coastal Ranges, NE Spain) are described for the first time. The Olorda Formation was studied in the Bruguers section, where two new tabulate coral species, Petridictyum casanovai n. sp. and Procteria �Granulidictyum�? gavaensis n. sp., have been collected. The �l Papiol Formation was studied in the �l Papiol and Cánoves sections, and four tabulate coral taxa, Sutherlandia? sp., Smythina humilis �Hinde, 1896�, Palaeacis sp. and Cladochonus sp., have been recognised. �n addition, the succession of the Olorda Formation in Bruguers is described. Lochkovian-lowermost Pragian age is established for the B Member of this formation in Bruguers and this section is correlated with the t��pe section of the formation in Santa Creu d'Olorda. Finall��, it is deduced that the sedimentation of the upper part �B Member� of the Olorda Formation, in Bruguers, and the �l Papiol Formation, in the �l Papiol, took place on a mudd�� and soft bottom, t��pical of still waters, with scarce terrigenous supplies.
Batalleria Revista De Paleontologia, 1997
Batalleria Revista De Paleontologia, 1994
Batalleria Revista De Paleontologia, 1996
Batalleria Revista De Paleontologia, 2002
Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especia... more Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especiament es fa l'estudi de les restes de Myliobatis aquila i de Pteromylauus bovinus. No hi ha distincio amb les especies actuals.
A level of grey-greenish shales, becoming yellow when weathered, which outcrops in the northern s... more A level of grey-greenish shales, becoming yellow when weathered, which outcrops in the northern slope of a track in Bruguès (W of Gava) yields a faunal assemblage of very small shells showing very close affinities with some bohemian Devonian assemblages. The fauna, which is indicative of a Lower Devonian age, is mainly composed of brachiopods which are typical of a BA4-5 position. The brachiopod fauna includes Orbiculoidea sp., Plectodonta (Plectodonta) mimica (Barrande), an undetermined strophochonetid chonetid, Jacetanella bruguesensis nov. gen., nov. sp., cf. Plicanoplites sp. and an undetermined (?) lissatrypid.
The sequence of early Lower Devonian (Lochkovian) strata with dominant anchimetamorphic shales of... more The sequence of early Lower Devonian (Lochkovian) strata with dominant anchimetamorphic shales of the Olorda Formation yielded numerous remains of eurypterids. These belong to the Family Pterygotidae and are represented by dominant species of ...
Batalleria Revista De Paleontologia, 2001
En el presente trabajo se cita por primera vez la presencia de Dombarites sp. En los materiales c... more En el presente trabajo se cita por primera vez la presencia de Dombarites sp. En los materiales carboniferos de El Papiol, por lo que deben referirse al transito Viseense-Namuriense.
Northeast Spain�. �Corales tabulados � � estratigraf�a del Dev�nico �nferior � � del Misis�pico e... more Northeast Spain�. �Corales tabulados � � estratigraf�a del Dev�nico �nferior � � del Misis�pico en las inmediaciones de Barcelona �Cordilleras Costeras Catalanas, nordeste de �spa�a�.] Revista Española de Paleontología, 22 �2�, 175-192. �SSN 0213-6937. �n this paper the content of tabulate corals of the Olorda �Lower Devonian � and �l Papiol �Mississipian � Forma-tions near Barcelona (Catalonian Coastal Ranges, NE Spain) are described for the first time. The Olorda Forma-tion was studied in the Bruguers section, where two new tabulate coral species, Petridictyum casanovai n. sp. and Procteria �Granulidictyum�? gavaensis n. sp., have been collected. The �l Papiol Formation was studied in the �l Papiol and Cánoves sections, and four tabulate coral taxa, Sutherlandia? sp., Smythina humilis �Hinde, 1896�, Palaeacis sp. and Cladochonus sp., have been recognised. �n addition, the succession of the Olorda Formation in Bruguers is described. Lochkovian-lowermost Pragian age is established f...
�n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Missis... more �n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Mississipian� Formations near Barcelona (Catalonian Coastal Ranges, NE Spain) are described for the first time. The Olorda Formation was studied in the Bruguers section, where two new tabulate coral species, Petridictyum casanovai n. sp. and Procteria �Granulidictyum�? gavaensis n. sp., have been collected. The �l Papiol Formation was studied in the �l Papiol and Cánoves sections, and four tabulate coral taxa, Sutherlandia? sp., Smythina humilis �Hinde, 1896�, Palaeacis sp. and Cladochonus sp., have been recognised. �n addition, the succession of the Olorda Formation in Bruguers is described. Lochkovian-lowermost Pragian age is established for the B Member of this formation in Bruguers and this section is correlated with the t��pe section of the formation in Santa Creu d’Olorda. Finall��, it is deduced that the sedimentation of the upper part �B Member� of the Olorda Formation, in Bruguers, an...
Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especia... more Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especiament es fa l'estudi de les restes de Myliobatis aquila i de Pteromylauus bovinus. No hi ha distincio amb les especies actuals.
Spanish Journal of Palaeontology, 2021
Se describe la sucesión estratigráfica del Carbonífero y se definen tres formaciones en varias lo... more Se describe la sucesión estratigráfica del Carbonífero y se definen tres formaciones en varias localidades situadas en el sector septentrional de las Cadenas Costeras Catalanas. Se estudian los braquiópodos de la Formación El Papiol en capas de edad próxima al límite Viseense-Serpukhoviense. Los braquiópodos son relativamente escasos y se encuentran casi exclusivamente como moldes internos o externos, con una conservación incompleta, lo que ha obligado a utilizar nomenclatura abierta. Se han identificado los siguientes taxones: Drahanorhynchus cf. paeckelmanni, Globosochonetes? sp. Parmephrix? cf. aprathensis, Chonetipustula cf. concentrica, Martinia sp., Tomiopsis? sp., Kitakamithyris? sp., Phricodothyris? sp. y Plicotorynifer? sp. Las asociaciones de braquiópodos son comparables a las del Viseense en facies Culm del norte de Europa, especialmente de Alemania. La relación también es grande con algunas formaciones carboníferas de la Cordillera Cantábrica, destacando el elevado númer...
Revista Espanola De Paleontologia, Apr 1, 2011
�n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Missis... more �n this paper the content of tabulate corals of the Olorda �Lower Devonian� and �l Papiol �Mississipian� Formations near Barcelona (Catalonian Coastal Ranges, NE Spain) are described for the first time. The Olorda Formation was studied in the Bruguers section, where two new tabulate coral species, Petridictyum casanovai n. sp. and Procteria �Granulidictyum�? gavaensis n. sp., have been collected. The �l Papiol Formation was studied in the �l Papiol and Cánoves sections, and four tabulate coral taxa, Sutherlandia? sp., Smythina humilis �Hinde, 1896�, Palaeacis sp. and Cladochonus sp., have been recognised. �n addition, the succession of the Olorda Formation in Bruguers is described. Lochkovian-lowermost Pragian age is established for the B Member of this formation in Bruguers and this section is correlated with the t��pe section of the formation in Santa Creu d'Olorda. Finall��, it is deduced that the sedimentation of the upper part �B Member� of the Olorda Formation, in Bruguers, and the �l Papiol Formation, in the �l Papiol, took place on a mudd�� and soft bottom, t��pical of still waters, with scarce terrigenous supplies.
Batalleria Revista De Paleontologia, 1997
Batalleria Revista De Paleontologia, 1994
Batalleria Revista De Paleontologia, 1996
Batalleria Revista De Paleontologia, 2002
Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especia... more Es descriuen els restes de fossils de Batoideus trobats al Plioce a la vora de Barcelona. Especiament es fa l'estudi de les restes de Myliobatis aquila i de Pteromylauus bovinus. No hi ha distincio amb les especies actuals.
A level of grey-greenish shales, becoming yellow when weathered, which outcrops in the northern s... more A level of grey-greenish shales, becoming yellow when weathered, which outcrops in the northern slope of a track in Bruguès (W of Gava) yields a faunal assemblage of very small shells showing very close affinities with some bohemian Devonian assemblages. The fauna, which is indicative of a Lower Devonian age, is mainly composed of brachiopods which are typical of a BA4-5 position. The brachiopod fauna includes Orbiculoidea sp., Plectodonta (Plectodonta) mimica (Barrande), an undetermined strophochonetid chonetid, Jacetanella bruguesensis nov. gen., nov. sp., cf. Plicanoplites sp. and an undetermined (?) lissatrypid.
The sequence of early Lower Devonian (Lochkovian) strata with dominant anchimetamorphic shales of... more The sequence of early Lower Devonian (Lochkovian) strata with dominant anchimetamorphic shales of the Olorda Formation yielded numerous remains of eurypterids. These belong to the Family Pterygotidae and are represented by dominant species of ...
Batalleria Revista De Paleontologia, 2001
En el presente trabajo se cita por primera vez la presencia de Dombarites sp. En los materiales c... more En el presente trabajo se cita por primera vez la presencia de Dombarites sp. En los materiales carboniferos de El Papiol, por lo que deben referirse al transito Viseense-Namuriense.