RT Journal Article
T1 Characterizing the sedimentary history of cave deposits, using archaeomagnetism and rock magnetism, Atapuerca (Northern Spain)
A1 Parés Casanova, J.M.
A1 Pérez González, Alfredo José
A1 Arsuaga Ferreras, Juan Luis
A1 Bermúdez de Castro, José María
A1 Carbonell, E.
A1 Ortega, A. I.
AB We use a combination of rock magnetism (anisotropy of magnetic susceptibility, AMS) and magnetic polarity to characterize cave deposits and as a proxy for sedimentary fabric. In three localities at the Atapuerca archaeological site (Galeria, Gran Dolina and Sala de los Cíclopes), magnetic foliation (K. max/K. int) is always greater than lineation (K. int/K. min), consistent with a primary, depositional, sedimentary fabric. Our results, although preliminary, reveal a higher degree of anisotropy in autochtonous deposits compared to allochthonous deposits, possibly indicative of a higher hydrodynamic regime in the former. At two localities the magnetic lineation (K. max) defines a cluster, which is thought to be antipodal to the palaeocurrent direction. Hence we are able to retrieve palaeoflow directions in deposits that otherwise lack any other sedimentary structure. We conclude that AMS is a powerful tool for determining the hydrodynamic character of depositional environments in cave sediments at the Atapuerca archaeological site. A better understanding of the depositional environment and how sedimentation occurred allows reconstruction of the karst evolution and ultimately a better definition of human interaction with the environment.
PB Wiley
SN 0003-813X,  online ISSN: 1475-4754
YR 2010
FD 2010-08
LK https://hdl.handle.net/20.500.14352/43528
UL https://hdl.handle.net/20.500.14352/43528
LA eng
NO Ministerio de Educación y Ciencia
DS Docta Complutense
RD 4 abr 2025