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<field name="value">Carrancho Alonso, Ángel</field>
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<field name="confidence">500</field>
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<field name="value">Villalaín Santamaria, Juan José</field>
<field name="authority">576</field>
<field name="confidence">500</field>
<field name="orcid_id">0000-0001-9948-0953</field>
<field name="value">Vallverdú, Josep</field>
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<field name="value">Carbonell, Eudald</field>
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<field name="confidence">600</field>
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<field name="value">2017-09-08T10:55:14Z</field>
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<field name="value">2018-09-01T02:45:06Z</field>
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<element name="none">
<field name="value">2016-09</field>
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<field name="value">1040-6182</field>
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<field name="value">10.1016/j.quaint.2015.12.083</field>
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<field name="value">Archaeomagnetic dating is probably one of the most known applications of magnetic methods to&#xd;
archaeology but there are others still underutilized and of particular interest to Palaeolithic archaeology.&#xd;
Here, we report a novel application of archaeomagnetism as a technique to determine temporal diachronies&#xd;
among combustion features from the same surface within palaeolithic palimpsests. The&#xd;
approach is based on the subtle directional changes of the Earth's magnetic field through time (secular&#xd;
variation, SV) and on the ability of burned materials to record such variations under certain conditions.&#xd;
Three Middle Palaeolithic hearths from level O (ca. 55 ka BP) at the Abric Romaní rock-shelter (NE Spain),&#xd;
were archaeomagnetically investigated. The studied surface (black homogeneous carbonaceous facies),&#xd;
recorded the magnetic enhancement produced by fire with a tenfold increase in concentrationdependent&#xd;
magnetic parameters in the uppermost centimetre with respect to its unburned or deeper&#xd;
counterparts. Pseudo-single domain (PSD) Ti-low titanomagnetite was identified as the main remanence&#xd;
carrier. The irreversibility of thermomagnetic curves suggests that these samples did not undergo&#xd;
enough high temperatures as to record a full thermoremanence (TRM). Additionally, the occasional&#xd;
occurrence of maghaemitized magnetite is interpreted as an indication of a thermochemical remanent&#xd;
magnetization (TCRM), making these samples unsuitable for absolute palaeointensity determinations.&#xd;
Two well-defined (a95 &lt; 5 ) and statistically indistinguishable archaeomagnetic directions were obtained&#xd;
with their mean directions within their respective confidences circles at the 95% level. The lack of&#xd;
directional changes and the similarity in the magnetic properties suggest that these hearths recorded&#xd;
simultaneously or closely confined in time the Earth's magnetic field direction at the time of cooling.&#xd;
These results agree well with archaeological evidence which indicates a synchronic occupation of this&#xd;
activity area. The possibility of determining temporal differences among combustion features in prehistoric&#xd;
sites arises as a promising tool in palimpsest dissection studies and may help to reconstruct&#xd;
occupation patterns of prehistoric groups. The practical limits of the method are discussed as well as its&#xd;
potential to identify post-depositional mechanical alteration processes.</field>
</element>
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<element name="sponsorship">
<element name="en">
<field name="value">Spanish Ministry of Economy and Competitiveness, (MINECO) and&#xd;
European Regional Development Fund (projects CGL2012-38481&#xd;
and CGL2012-32149)</field>
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<element name="es">
<field name="value">eng</field>
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<element name="publisher">
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<field name="value">Elsevier</field>
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<field name="value">Quaternary International. 2016, V. 417, p. 39-50</field>
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<field name="value">https://doi.org/10.1016/j.quaint.2015.12.083</field>
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<field name="value">Attribution-NonCommercial-NoDerivatives 4.0 International</field>
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<element name="subject">
<element name="en">
<field name="value">Archaeomagnetism</field>
<field name="value">Diachrony</field>
<field name="value">Hearth</field>
<field name="value">Middle Palaeolithic</field>
<field name="value">Neanderthals</field>
<field name="value">Secular variation</field>
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<element name="en">
<field name="value">Physics</field>
<field name="value">Paleontology</field>
</element>
<element name="es">
<field name="value">Física</field>
<field name="value">Paleontología</field>
</element>
</element>
</element>
<element name="title">
<element name="en">
<field name="value">Is it possible to identify temporal differences among combustion features in Middle Palaeolithic palimpsests? The archaeomagnetic evidence: A case study from level O at the Abric Romaní rock-shelter (Capellades, Spain)</field>
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