Zobrazeno 1 - 10
of 63
pro vyhledávání: '"Peter W. Skelton"'
Publikováno v:
Geologia Croatica, Vol 56, Iss 2, Pp 139-148 (2003)
The requieniid rudist species ‘Matheronia’ salevensis FAVRE, first described from the Tithonian of Mont Salève, eastern France, is transferredto the genus Hypelasma PAQUIER, which is distinguished from Matheronia by possession of a posterior myo
Externí odkaz:
https://doaj.org/article/8a6a82b37308466eb8587925acac8d46
Autor:
Rafael Martínez-Rodríguez, Luis M. Nieto, José M. Castro, Ginés A. de Gea, Pedro A. Ruiz-Ortiz, José M. Molina, Peter W. Skelton
The Middle Member of the Llopis Fm in the Sierra de Bedmar-Jódar Unit of the Prebetic Zone of Jaén (southern Spain) was deposited on a shallow-marine platform of the Southern Iberian Continental Margin during the earliest Aptian. Detailed field log
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::790cd69ed4cb6ee654c7a53a5c1a8352
https://eprints.ucm.es/id/eprint/78187/
https://eprints.ucm.es/id/eprint/78187/
Autor:
Helmut Weissert, Richard D. Pancost, Luis M. Nieto, Matías Reolid, María Luisa Quijano, P. A. Ruiz-Ortiz, Peter W. Skelton, Rafael Martínez-Rodríguez, José Miguel Molina, Ian Jarvis, Carmina López-Rodríguez, José Manuel Castro, Ginés A. de Gea, Roque Aguado
Publikováno v:
Paleoceanography and Paleoclimatology
Castro, J M, Ruiz-Ortiz, P A, de Gea, G A, Aguado, R, Jarvis, I, Weissert, H, Molina, J M, Nieto, L M, Pancost, R D, Quijano, M L, Reolid, M, Skelton, P W, López-Rodríguez, C & Martínez-Rodríguez, R 2021, ' High-Resolution C-isotope, TOC and Biostratigraphic Records of OAE1a (Aptian) from an Expanded Hemipelagic Cored Succession, Western Tethys : a New Stratigraphic Reference for Global Correlation and Paleoenvironmental Reconstruction ', Paleoceanography and Paleoclimatology, vol. 36, no. 3, e2020PA004004 . https://doi.org/10.1029/2020PA004004
Castro, J M, Ruiz-Ortiz, P A, de Gea, G A, Aguado, R, Jarvis, I, Weissert, H, Molina, J M, Nieto, L M, Pancost, R D, Quijano, M L, Reolid, M, Skelton, P W, López-Rodríguez, C & Martínez-Rodríguez, R 2021, ' High-Resolution C-isotope, TOC and Biostratigraphic Records of OAE1a (Aptian) from an Expanded Hemipelagic Cored Succession, Western Tethys : a New Stratigraphic Reference for Global Correlation and Paleoenvironmental Reconstruction ', Paleoceanography and Paleoclimatology, vol. 36, no. 3, e2020PA004004 . https://doi.org/10.1029/2020PA004004
A high-resolution carbonate C-isotope stratigraphy for the Aptian is presented for the Cau core (Spain). The biostratigraphically calibrated C-isotope stratigraphy of the core is used to refine the previously defined C-isotope segments of the Aptian.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6b162fb3c17cec367a6e84908d875a44
https://eprints.kingston.ac.uk/id/eprint/48338/11/Jarvis-I-48338-VoR.pdf
https://eprints.kingston.ac.uk/id/eprint/48338/11/Jarvis-I-48338-VoR.pdf
Autor:
Peter W. Skelton, Yichun Zhang, Xin Rao, Zhaoxiong Ma, Bo Peng, Yanhong Pan, Shin–ichi Sano, Yiqiang Zhang, Tong Zhang, Huawei Cai
A new polyconitid rudist Shajia tibetica gen. et sp. nov., of late Aptian to Albian age, is described from the Langshan Formation of Nyima County, northern Lhasa Block, Tibet. Though comparable in size and external morphology with Horiopleura haydeni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea786dc049ee35df3b375055daf4f89c
http://oro.open.ac.uk/61661/1/1-s2.0-S0195667118303501-main.pdf
http://oro.open.ac.uk/61661/1/1-s2.0-S0195667118303501-main.pdf
Publikováno v:
Spanish Journal of Palaeontology. 11:172
En ambos flancos de! anticlinal de Sant Corneli, en la unidad central surpirenaica, afloran facies de plataforma calcárea de edad Santoniense. En este trabajo, hemos realizado un análisis paleoambiental detallado de la formación de rudistas y cora
Autor:
Shin-ichi Sano, Cai Li, Bo Peng, Hui Luo, Huawei Cai, Xin Rao, Peter W. Skelton, Jingeng Sha, Yanhong Pan
Publikováno v:
Papers in Palaeontology. 3:297-315
Diagnostic characters of the recently established new genus of radiolitid rudist Auroradiolites include an entirely compact outer shell layer, a distinctly convex upper (left) valve and a robust myocardinal apparatus surrounding a strongly internally
Publikováno v:
BSGF-Earth Sciences Bulletin, Vol 190, p 3 (2019)
The Aptian stratigraphic record of the Alicante region consists of: a rudist and coral-rich carbonate platform of earliest Aptian age (Llopis Formation), with a discontinuous siliciclastic member at its top; followed by late Early, to Late Aptian hem
Publikováno v:
Advances in Science, Technology & Innovation ISBN: 9783030014513
The background to the preparation of the rudist sections for the ongoing complete revision of the Bivalvia volumes of the ‘Treatise on Invertebrate Palaeontology’ is described. The progress on publication is reported. The plans for further work a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::341bf70fc9f6428336d2f3ed7eb644d4
https://doi.org/10.1007/978-3-030-01452-0_6
https://doi.org/10.1007/978-3-030-01452-0_6
Publikováno v:
Advances in Science, Technology & Innovation ISBN: 9783030014513
This investigation is aimed to study the morphological variability of the polyconitid rudist, Polyconites hadriani, from the Aptian carbonate platforms of the western Maestrat Basin, in Iberia. The individuals of the platform top to upper slope carbo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e48a8f97e352a56efa0def65a67388fd
https://doi.org/10.1007/978-3-030-01452-0_7
https://doi.org/10.1007/978-3-030-01452-0_7
Publikováno v:
Advances in Science, Technology & Innovation ISBN: 9783030014513
A total of four rudist taxa had been distinguished from the Sangzugang Formation and the Langshan Formation of the Lhasa block, Tibet by Rao et al. [4, 5]. They are Auroradiolites biconvexus [5], Magallanesia rutogensis [5], Eoradiolites cf. hedini a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c49dbb9783387db9c202c29193f443d
https://doi.org/10.1007/978-3-030-01452-0_22
https://doi.org/10.1007/978-3-030-01452-0_22