Phanerozoic stromatolites II Libro electrónico

Precambrian stromatolites have received in depth, consideration from geologists and paleontologists; they were indeed searching for biosedimentary structures that were sufficiently characteristic and widely distributed to be considered as useful tools for stratigraphic correlation. Silicified stromatolites are also of interest as they contain preserved traces of ancient life. Calcareous Phanerozoic stromatolites have not received very much attention from geologists. Logan's too schematic morphological classification of 1964, was not so helpful to the knowledge of Phanerozoic stromatolites because neither their morphology nor their microstructure were studied in the same detail in which Proterozoic stromatolites have now been described. We therefore know little about the Phanerozoic stromatolites which, do, however, show an interesting range of diversification. A major questions stiII remaining to be answered include the history of stromatolite development and wether their morphology has "evolved" in addition to detailed information concerning Cenozoic nonmarine stromatolites which precipitate carbonate and the Recent giant stromatolites which trap particles. For these reasons Claude Monty, in 1981, launched the first volume of what was going to be a series on "Phanerozoic stromatolites" in order to describe their morphology, microstructure and paleoecology and to present them in their stratigraphic context.

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Main Authors: Bertrand-Sarfati, Janine editor, Monty, Claude editor
Format: Texto biblioteca
Language:eng
Published: Dordrecht Springer c199
Online Access:http://link.springer.com/book/10.1007%2F978-94-011-1124-9
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spelling KOHA-OAI-ECOSUR:570842021-01-11T22:02:50ZPhanerozoic stromatolites II Libro electrónico Bertrand-Sarfati, Janine editor Monty, Claude editor textDordrecht Springerc1994engPrecambrian stromatolites have received in depth, consideration from geologists and paleontologists; they were indeed searching for biosedimentary structures that were sufficiently characteristic and widely distributed to be considered as useful tools for stratigraphic correlation. Silicified stromatolites are also of interest as they contain preserved traces of ancient life. Calcareous Phanerozoic stromatolites have not received very much attention from geologists. Logan's too schematic morphological classification of 1964, was not so helpful to the knowledge of Phanerozoic stromatolites because neither their morphology nor their microstructure were studied in the same detail in which Proterozoic stromatolites have now been described. We therefore know little about the Phanerozoic stromatolites which, do, however, show an interesting range of diversification. A major questions stiII remaining to be answered include the history of stromatolite development and wether their morphology has "evolved" in addition to detailed information concerning Cenozoic nonmarine stromatolites which precipitate carbonate and the Recent giant stromatolites which trap particles. For these reasons Claude Monty, in 1981, launched the first volume of what was going to be a series on "Phanerozoic stromatolites" in order to describe their morphology, microstructure and paleoecology and to present them in their stratigraphic context.Incluye bibliografíaPrecambrian stromatolites have received in depth, consideration from geologists and paleontologists; they were indeed searching for biosedimentary structures that were sufficiently characteristic and widely distributed to be considered as useful tools for stratigraphic correlation. Silicified stromatolites are also of interest as they contain preserved traces of ancient life. Calcareous Phanerozoic stromatolites have not received very much attention from geologists. Logan's too schematic morphological classification of 1964, was not so helpful to the knowledge of Phanerozoic stromatolites because neither their morphology nor their microstructure were studied in the same detail in which Proterozoic stromatolites have now been described. We therefore know little about the Phanerozoic stromatolites which, do, however, show an interesting range of diversification. A major questions stiII remaining to be answered include the history of stromatolite development and wether their morphology has "evolved" in addition to detailed information concerning Cenozoic nonmarine stromatolites which precipitate carbonate and the Recent giant stromatolites which trap particles. For these reasons Claude Monty, in 1981, launched the first volume of what was going to be a series on "Phanerozoic stromatolites" in order to describe their morphology, microstructure and paleoecology and to present them in their stratigraphic context.Disponible en formato PDFSubscripción a ELSEVIERDisponible en líneahttp://link.springer.com/book/10.1007%2F978-94-011-1124-9URN:ISBN:9401044910URN:ISBN:9789401044912URN:ISBN:9789401111249 (Online)Disponible para usuarios de ECOSUR con su clave de acceso
institution ECOSUR
collection Koha
country México
countrycode MX
component Bibliográfico
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databasecode cat-ecosur
tag biblioteca
region America del Norte
libraryname Sistema de Información Bibliotecario de ECOSUR (SIBE)
language eng
description Precambrian stromatolites have received in depth, consideration from geologists and paleontologists; they were indeed searching for biosedimentary structures that were sufficiently characteristic and widely distributed to be considered as useful tools for stratigraphic correlation. Silicified stromatolites are also of interest as they contain preserved traces of ancient life. Calcareous Phanerozoic stromatolites have not received very much attention from geologists. Logan's too schematic morphological classification of 1964, was not so helpful to the knowledge of Phanerozoic stromatolites because neither their morphology nor their microstructure were studied in the same detail in which Proterozoic stromatolites have now been described. We therefore know little about the Phanerozoic stromatolites which, do, however, show an interesting range of diversification. A major questions stiII remaining to be answered include the history of stromatolite development and wether their morphology has "evolved" in addition to detailed information concerning Cenozoic nonmarine stromatolites which precipitate carbonate and the Recent giant stromatolites which trap particles. For these reasons Claude Monty, in 1981, launched the first volume of what was going to be a series on "Phanerozoic stromatolites" in order to describe their morphology, microstructure and paleoecology and to present them in their stratigraphic context.
format Texto
author Bertrand-Sarfati, Janine editor
Monty, Claude editor
spellingShingle Bertrand-Sarfati, Janine editor
Monty, Claude editor
Phanerozoic stromatolites II Libro electrónico
author_facet Bertrand-Sarfati, Janine editor
Monty, Claude editor
author_sort Bertrand-Sarfati, Janine editor
title Phanerozoic stromatolites II Libro electrónico
title_short Phanerozoic stromatolites II Libro electrónico
title_full Phanerozoic stromatolites II Libro electrónico
title_fullStr Phanerozoic stromatolites II Libro electrónico
title_full_unstemmed Phanerozoic stromatolites II Libro electrónico
title_sort phanerozoic stromatolites ii libro electrónico
publisher Dordrecht Springer
publishDate c199
url http://link.springer.com/book/10.1007%2F978-94-011-1124-9
work_keys_str_mv AT bertrandsarfatijanineeditor phanerozoicstromatolitesiilibroelectronico
AT montyclaudeeditor phanerozoicstromatolitesiilibroelectronico
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