The significance of stable isotopes as dietary indicators in ancient terrestrial...
The significance of stable isotopes as dietary indicators in ancient terrestrial ecosystems
"Paleodietary reconstruction is an important component of palaeoecology, but evidence for diet of ancient organisms is very rare and mostly limited to indirect inference. Besides, our knowledge related to the trophic organization...
ver más
¿Tienes un proyecto y buscas un partner? Gracias a nuestro motor inteligente podemos recomendarte los mejores socios y ponerte en contacto con ellos. Te lo explicamos en este video
Proyectos interesantes
I-GOAT
Isotopic fractionation in goats effects of diet diet quali...
191K€
Cerrado
CGL2009-13159
OSTRACODOS SUBFOSILES EN SEDIMENTOS LACUSTRES CUATERNARIOS:...
4K€
Cerrado
CGL2010-19825
PROCESOS TAFONOMICOS: REPERCUSION EN INTERPRETACIONES PALEOE...
145K€
Cerrado
ITALIAN ISOTOPES
Stable isotope ecology of hunter gatherers in Italy in the l...
167K€
Cerrado
HAR2010-22115-C02-02
APLICACION DEL ANALISIS DE SUSTANCIAS ORGANICAS E INORGANICA...
54K€
Cerrado
CGL2011-30141
MODELO CLIMATICO PARA EL CUATERNARIO SUPERIOR DEL NOROESTE D...
114K€
Cerrado
Información proyecto SSIDIATE
Líder del proyecto
UNIVERSITY OF BRISTOL
No se ha especificado una descripción o un objeto social para esta compañía.
TRL
4-5
Presupuesto del proyecto
200K€
Fecha límite de participación
Sin fecha límite de participación.
Descripción del proyecto
"Paleodietary reconstruction is an important component of palaeoecology, but evidence for diet of ancient organisms is very rare and mostly limited to indirect inference. Besides, our knowledge related to the trophic organization of extinct communities mostly relies on assumptions from morphofunctional studies. Contrary to living communities, quantitative assessment of the trophic relationships within a given extinct ecosystem remains virtually unexplored and represents a key to discuss ecosystem dynamics across major events that affected the biosphere through time. The current proposal will determine the diet of unstudied ancient organisms through chemical isotopic systems.
Biological processes such as digestion, cell growth or enzyme production involve important isotopic fractionations of various elements assimilated through food consumption or water uptake. This observed shift between a food source (plants for example) and the consumer's organs is linked to the fractionation of stable isotopes during nutrient uptake into the intestinal cells.
Here, the study will focus on the trophic chain hierarchy of large Cretaceous and extant terrestrial vertebrates involving : carbon, a consituent of mineralized tissue used for trophic inference, mostly in mammals; calcium, constituting up to half the apatite (the key mineralised constituent of bones and teeth) and for which preliminary investigations suggest a fractionation; magnesium, one of the most abundant element involved in metabolism and for which fractionation remains unexplored. The analyses will focus on tooth enamel apatite, the most susceptible body part to be preserved in the fossil record and to retain its pristine signal. The following project therefore intends to define appropriate proxies in living organisms that will serve as a basis to explore isotopic variability among the succession of ancient communities through time."