Zobrazeno 1 - 10
of 159
pro vyhledávání: '"Juan C. Braga"'
Autor:
Juan C. Braga, Julio Aguirre
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Rhodolith limestones occur in the upper part of the Miocene infill of the Ronda Basin in southern Spain. This basin was an embayment at the southern margin of the Atlantic-linked Guadalquivir Basin, the foreland basin of the Betic Cordillera. Messini
Externí odkaz:
https://doaj.org/article/6b0bc9f721a3441c88e137b167404d61
Autor:
Julio Aguirre, Juan C. Braga
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Serravallian (middle Miocene) coralline algal assemblages at the southern margin of the Guadalquivir Basin (southern Spain) occur as rhodoliths preserved in situ or very close to their growth habitats (autochthonous–parautochthonous assemblages) an
Externí odkaz:
https://doaj.org/article/f0f8853d81ed40ebb4a5bfa6577ccba8
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
During the Paleocene/Eocene Thermal Maximum, ~55.6 Ma, the Earth experienced the warmest event of the last 66 Ma due to a massive release of CO2. This event lasted for ~100 thousands of years with the consequent ocean acidification (estimated pH = 7.
Externí odkaz:
https://doaj.org/article/5db45ca2a51340889230d10566b651e4
Autor:
Davide Bassi, Juan C. Braga, Masato Owada, Julio Aguirre, Jere H. Lipps, Hideko Takayanagi, Yasufumi Iryu
Publikováno v:
Progress in Earth and Planetary Science, Vol 7, Iss 1, Pp 1-17 (2020)
Abstract Macroids and rhodoliths, made by encrusting acervulinid foraminifera and coralline algae, are widely recognized as bioengineers providing relatively stable microhabitats and increasing biodiversity for other species. Macroid and rhodolith be
Externí odkaz:
https://doaj.org/article/bf98c19a106842f9be089211e0a337f9
Autor:
Nicholas F. L. Vale, Juan C. Braga, Alex C. Bastos, Fernando C. Moraes, Claudia S. Karez, Ricardo G. Bahia, Luis A. Leão, Renato C. Pereira, Gilberto M. Amado-Filho, Leonardo T. Salgado
Publikováno v:
Diversity, Vol 14, Iss 4, p 282 (2022)
Rhodolith beds are biogenic benthic habitats mainly formed by unattached, non-geniculate coralline algae, which can be inhabited by many associated species. The Brazilian continental shelf encompasses the largest continuous rhodolith bed in the world
Externí odkaz:
https://doaj.org/article/1bd60d0e71e64fa290c96f3a53af4ff9
Autor:
Fabio Rindi, Juan C. Braga, Sophie Martin, Viviana Peña, Line Le Gall, Annalisa Caragnano, Julio Aguirre
Publikováno v:
Frontiers in Marine Science, Vol 6 (2019)
In this review we assess the state of knowledge for the coralline algae of the Mediterranean Sea, a group of calcareous seaweeds imperfectly known and considered highly vulnerable to long-term climate change. Corallines have occurred in the Mediterra
Externí odkaz:
https://doaj.org/article/27fd4b952ca142649cf310c3c0c3cc57
Autor:
Julio Aguirre, Juan C. Braga, Victoriano Pujalte, Xabier Orue-Etxebarria, Edward Salazar-Ortiz, Daniel Rincón-Martínez, Manuel Abad, Fernando Pérez-Valera
Publikováno v:
Diversity, Vol 12, Iss 3, p 117 (2020)
During the greenhouse conditions prevailing in the early−middle Eocene, larger benthic foraminifers (LBF) spread out on carbonate platforms worldwide while rhodolith beds were scarcely represented. This reduction in rhodolith beds coincided with a
Externí odkaz:
https://doaj.org/article/8b1748e8b3874ca7baf2dea03c508516
Publikováno v:
Coral Reefs and Sea-Level Change: Quaternary Records and Modelling. :1-38
Corals, coralline algae and vermetid gastropods are indirect (marine limiting) relative sea-level (RSL) indicators. The precision in sea-level reconstruction based on fossils of those organisms depends on the probable palaeodepth in which they grew.
Publikováno v:
Journal of Sedimentary Research. 92:257-274
While spatial facies patterns can be observed in modern systems, only vertical facies successions can usually be examined in ancient deposits. Lateral facies relationships (depositional models) and relative sea-level changes throughout time are tradi
Autor:
Davide Bassi, Monica Bolivar-Feriche, Willem Renema, Juan C. Braga, Johannes Pignatti, Giovanni Di Domenico, Kazuhiko Fujita, Jere H. Lipps, Jesús Reolid, Yasufumi Iryu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6169e7803c87fab2b3da50e7bc2fce98
http://hdl.handle.net/11573/1633082
http://hdl.handle.net/11573/1633082