Plant tissue decay in long-term experiments with microbial mats

The sequence of decay in fern pinnules was tracked using the species Davallia canariensis. Taphonomic alterations in the sediment–water interface (control tanks) and in subaqueous conditions with microbial mats were compared. The decay sequences were similar in control and mat tanks; in both cases,...

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Detalles Bibliográficos
Autores: Iniesto, Miguel, Blanco Moreno, Candela, Villalba, Aurora, Delgado Buscalioni, Ángela, Guerrero, M. Carmen, López Archilla, Ana Isabel
Tipo de recurso: artículo
Fecha de publicación:2018
País:España
Institución:Universidad Autónoma de Madrid
Repositorio:Biblos-e Archivo. Repositorio Institucional de la UAM
Idioma:inglés
OAI Identifier:oai:repositorio.uam.es:10486/690861
Acceso en línea:http://hdl.handle.net/10486/690861
https://dx.doi.org/10.3390/geosciences8110387
Access Level:acceso abierto
Palabra clave:Biomineralization
Experimental taphonomy
Plant decay
Plant fossilization
Soft-tissue preservation
Biología y Biomedicina / Biología
Descripción
Sumario:The sequence of decay in fern pinnules was tracked using the species Davallia canariensis. Taphonomic alterations in the sediment–water interface (control tanks) and in subaqueous conditions with microbial mats were compared. The decay sequences were similar in control and mat tanks; in both cases, pinnules preserved the shape throughout the four-month experience. However, the quality and integrity of tissues were greater in mats. In control tanks, in which we detected anoxic and neutral acid conditions, the appearance of a fungal–bacterial biofilm promoted mechanical (cell breakage and tissue distortions) and geochemical changes (infrequent mineralizations) on the external and internal pinnule tissues. In mats, characterized by stable dissolved oxygen and basic pH, pinnules became progressively entombed. These settings, together with the products derived from mat metabolisms (exopolymeric substances, proteins, and rich-Ca nucleation), promoted the integrity of external and internal tissues, and favored massive and diverse mineralization processes. The experience validates that the patterns of taphonomic alterations may be applied in fossil plants