Search

We present new paleomagnetic and rock magnetic data from mid and late Holocene sediments recovered in two gravity cores (C087 and C142a) from Lake Issyk-Kul (central Asia), for which independent radiocarbon-based age models are available. Our results indicate that sediments from core C087 are characterized by fine (pseudo single domain) magnetite grains and are reliable recorders of Holocene geomagnetic paleosecular variation (PSV) in central Asia, which is a region with poor data coverage. Similarity is found between the core C087 PSV record, which spans the last 5700 years, and the Lake Baikal PSV record, which is the only published Holocene central Asian PSV record of comparable length with an independent radiocarbon-based chronology. Our new results represent a step forward in constructing a reference PSV curve for central Asia that can be used to date sedimentary sequences. These results can also be used to improve the reliability and accuracy of global geomagnetic field models. We have not been able to disentangle past environmental changes in the Lake Issyk-Kul region based on rock magnetic properties, probably because the magnetite and hematite in the studied sediments have a mixed (fluvial and eolian) terrigenous origin. Copyright 2012 by the American Geophysical Union., Financial support for this research was provided through a CSIC JAE-Doc post-doctoral research contract (MGP), the GRACCIE (Spanish Consolider-Ingenio CSD2007-00067), APELIK (EU ICA2-CT-2000-10003), CGL2008-02203/BTE, and PALEONAO (CGL2010-15767/BTE) research projects.

Archaeomagnetic data indicate that during the past 2500 years there have been periods of rapid geomagnetic field intensity fluctuations interspersed with periods of almost constant field strength. The occurrence and the behaviour of these changes are under discussion and the challenge now is to precisely describe them. The aim of this study is to obtain an improved description of the sharp geomagnetic intensity change that took place in Western Europe around 800 AD. For this purpose 13 precisely dated early medieval Spanish pottery fragments, 4 archaeological French kilns and 3 collections of bricks used for the construction of different French historical buildings with ages ranging between 330 and 1260 AD have been studied. Classical Thellier experiments performed on 164 specimens, and including anisotropy of thermoremanent magnetisation and cooling rate corrections, gave 119 reliable results. The ten new high-quality mean archaeointensities obtained together with previously published data from Western Europe that we deem to be the most reliable, confirm the existence of an intensity maximum of ~85 ¿T centred at ~800 AD and related to intensity changes up to 25 ¿T per century. The new data also suggest that a previous abrupt intensity change occurred in Western Europe around 625 AD., Financial support was given by a CSIC JAE-Doc postdoctoral research contract (MGP), by the CGL2008-02203/BTE, CGL2011-24790, and CGL2010-15767/BTE research projects from the Spanish ministry of Science and Innovation

In this work, we present 16 directional and 27 intensity high‐quality values from Iberia. Moreover, we have updated the Iberian archeomagnetic catalogue published more than 10 years ago with a considerable increase in the database. This has led to a notable improvement of both temporal and spatial data distribution. A full vector paleosecular variation curve from 1000 BC to 1900 AD has been developed using high‐quality data within a radius of 900 km from Madrid. A hierarchical bootstrap method has been followed for the computation of the curves. The most remarkable feature of the new curves is a notable intensity maximum of about 80 μT around 600 BC, which has not been previously reported for the Iberian Peninsula. We have also analyzed the evolution of the paleofield in Europe for the last three thousand years and conclude that the high maximum intensity values observed around 600 BC in the Iberian Peninsula could respond to the same feature as the Levantine Iron Age Anomaly, after travelling westward through Europe., Authors acknowledge the Spanish Ministry of Economy (CGL2014-54112-R and CGL2017-87015-P projects; BES-2015- 074575 and BES-2016-077257 grants), the Spanish Ministry of Education (FPU14/02422 grant), and the Autonomous Community of Madrid through the European Youth Employment Initiative (PEJ15/AMB/AI- 0203). M. G. P. and M. R. acknowledge the Ramón y Cajal program and the CGL2015-63888-R project of the Spanish Ministry of Economy and Competitiveness. Financial support was also given by the PICS International Program for Scientific Cooperation (CNRS-France and CSIC-Spain).