09false100true score desc 2gaptrue5mapcontentxmltrue50object_type_i,object_type_i_lookup,coverage_period_mt,geographic_area_mt,geographic_coordinates_mt,author_role_mt,contributor_role_mt,org_id_mt,org_role_mt,supervisor_mt,supervisor_id_mi,supervisor_id_mi_lookup,fields_of_research_mi,fields_of_research_mi_lookup,display_type_i,display_type_i_lookup,seo_code_mi,seo_code_mi_lookup,copyright_i,license_i,license_i_lookup,oa_compliance_t,oa_notes_t,grant_id_t,funding_body_t,description_of_resource_t,software_required_t,project_description_t,keywords_mt,project_name_t,project_id_t,isdatasetof_mt,isdatasetof_mt_lookup,notes_t,date_dt,xsd_display_option_mi,xsd_display_option_mi_lookup,file_downloads_i,created_date_dt,updated_date_dt,research_program_mt,title_t,depositor_i,isderivationof_mt,assigned_user_id_mt,assigned_group_id_mi,assigned_group_id_mi_lookup,isdatacomponentof_mt,isannotationof_mt,author_id_mi,author_id_mi_lookup,alternative_title_mt,pid_t,publisher_t,author_mt,contributor_mt,contributor_id_mi,contributor_id_mi_lookup,refereed_i,series_t,journal_name_t,newspaper_t,conference_name_t,book_title_t,identifier_mt,edition_t,subject_mi,subject_mi_lookup,place_of_publication_t,start_page_t,end_page_t,chapter_number_t,issue_number_t,volume_number_t,conference_dates_t,conference_location_t,patent_number_t,country_of_issue_t,description_t,date_available_dt,language_mt,phonetic_title_t,language_of_title_mt,translated_title_t,phonetic_journal_name_t,translated_journal_name_t,phonetic_book_title_t,translated_book_title_t,phonetic_newspaper_t,file_attachment_name_mt,translated_newspaper_t,phonetic_conference_name_t,translated_conference_name_t,issn_mt,isbn_mt,isi_loc_t,prn_t,output_availability_t,na_explanation_t,sensitivity_explanation_t,file_attachment_content_mt,org_unit_name_t,org_name_t,report_number_t,sequence_i,genre_t,genre_type_t,formatted_title_t,formatted_abstract_t,parent_publication_t,convener_t,ismemberof_mt,ismemberof_mt_lookup,link_mt,link_description_mt,rights_t,views_i,scopus_id_t,thomson_citation_count_i,gs_citation_count_i,gs_cited_by_link_t,scopus_citation_count_i,status_i,status_i_lookup,first_author_in_document_derived_t,first_author_in_fez_derived_t,ands_collection_type_t,start_date_dt,end_date_dt,access_conditions_t,extent_t,contact_details_email_mt,contact_details_physical_mt,loc_subject_heading_mt,depositor_affiliation_i,surrounding_features_mt,condition_mt,style_mt,period_mt,category_mt,subcategory_mt,structural_systems_mt,adt_id_t,subtype_t,language_of_parent_title_t,proceedings_title_t,file_description_mt,herdc_code_i,herdc_code_i_lookup,herdc_status_i,herdc_status_i_lookup,institutional_status_i,institutional_status_i_lookup,herdc_notes_t,follow_up_flags_i,follow_up_flags_i_lookup,follow_up_flags_imu_i,follow_up_flags_imu_i_lookup,scopus_doc_type_t,scopus_doc_type_t_lookup,wok_doc_type_t,wok_doc_type_t_lookup,conference_id_i,total_chapters_t,publisher_id_i,translated_proceedings_title_t,native_script_title_t,roman_script_title_t,native_script_book_title_t,roman_script_book_title_t,native_script_journal_name_t,roman_script_journal_name_t,native_script_conference_name_t,roman_script_conference_name_t,total_pages_t,native_script_proceedings_title_t,roman_script_proceedings_title_t,language_of_book_title_mt,language_of_journal_name_mt,language_of_proceedings_title_mt,doi_t,author_count_t,collection_year_dt,location_mt,building_materials_mt,architectural_features_mt,interior_features_mt,sherpa_colour_t,ain_detail_t,rj_2010_rank_t,rj_2010_title_t,rj_2012_rank_t,rj_2012_title_t,rc_2010_rank_t,rc_2010_title_t,herdc_code_description_t,score,citation_t1true60 (indicator AND date_dt: [2000\-01\-01T00\:00\:00Z TO 2000\-12\-31T00\:00\:00Z] AND author_mt:(Harrold, Francis B) AND display_type_i:423 AND status_i:(2)) 6display_type_idisplay_type_i_lookup_exactkeywords_mftdate_year_tauthor_id_miauthor_id_mi_lookup_exactauthor_mftjournal_name_t_ftsubject_misubject_mi_lookup_exactgenre_type_t_ftismemberof_mftismemberof_mt_lookup_exactsubtype_t_ftscopus_doc_type_t_ftscopus_doc_type_t_lookup_exact(_authlister_t:(1)) AND (status_i:(2)) 34232000-01-01T00:00:00Z14052008-03-26T23:43:09ZThe view from across the Pyrenees : changing perspectives on the Middle/Upper Paleolithic transition in Spanish Prehistorybibliuned:ETFSerie1-B1EE16F0-EC1F-4F1A-19AD-807C6F40EEF7La comprension de la transiclon del
Paleolitico Medio al Superior ha
cambiado entre los prehistoriadores que
han trabajado en Espana durante el
ultimo siglo. Muchos investigadores han
asociado esta transicion con el
reemplazamiento de los Neandertales por
los humanos anatomicamente modemos,
aunque en el contexto de las persistentes
diferencias sobre la naturaleza y
extension de los movimientos
poblacionales y las influencias culturales
en Espana desde el Norte de Africa o
desde Francia. La Informacion
arqueologica es de una calidad y cantidad
sin precedentes. Sin embargo entre las
indicaciones de una temprana aparicion
del Aurihadense en el Norte de Espana y
la persistencia, hasta fechas muy tardfas
del Musteriense en el Sur, existe un
considerable desacuerdo sobre la
naturaleza de la transicion Paleolitico
Medio-Superior en la peninsula.Understandings of the Middle-Upper
Paleolithic transition by prehistorians
working in Spain have changed in the
course of the last century. Most workers
have associated this transition with the
replacement of Neanderthals by
anatomically modern humans, although
in the context of persistent
disagreements over the nature and
extent of movements of populations
and cultural influences into Spain from
North Africa and from France. The
current relevant archaeological database
is of unprecedented quality and quantity.
However, in the wake of indications of
an early appearance of the Aurignacian
in northern Spain, and the late
persistence of the Mousterian and
Neanderthals in southern Spain and
Portugal, there is currently considerable
disagreement over the nature of the
Middle-Upper Paleolithic transition in the
peninsula.07052<a class="citation_author_name" title="Browse by Author Name for Harrold, Francis B." href="/fez/list/author/Harrold, Francis B./">Harrold, Francis B.</a> . (<span class="citation_date">2000</span>) <a class="citation_title" title="Click para ver : The view from across the Pyrenees : changing perspectives on the Middle/Upper Paleolithic transition in Spanish Prehistory" href="/fez/view/bibliuned:ETFSerie1-B1EE16F0-EC1F-4F1A-19AD-807C6F40EEF7">The view from across the Pyrenees : changing perspectives on the Middle/Upper Paleolithic transition in Spanish Prehistory</a>. RecordArtículo de revistaPublishedhttp://udcdata.info/068273HistoriaUniversidad Nacional de Educación a Distancia (España). Facultad de Geografía e HistoriaHarrold, Francis B.bibliuned:ETFSerie1-B1EE16F0-EC1F-4F1A-19AD-807C6F40EEF7http://e-spacio.uned.es/fez/view/bibliuned:ETFSerie1-B1EE16F0-EC1F-4F1A-19AD-807C6F40EEF7spaDocumento.pdfbibliuned:ETFSerieI2000bibliuned:Setopenairebibliuned:SetarticuloEspacio, tiempo y forma. Serie I, Prehistoria y arqueología. Año 2000, n. 13Set de openaireSet de artículohttp://creativecommons.org/licenses/by-nc-nd/4.0Licencia Creative CommonsHarroldAcceso abierto7.082348334232000-01-01T00:00:00Z5652008-03-26T23:45:06ZA Test of the MSEC Method for Paleoclimate and intersite correlations from Late Pleistocene/Holocene cave sites in southern Europe : results from Cova de les Cendres, SE Spainbibliuned:ETFSerie1-2255AB0C-94DE-3638-B963-46D270E6689AEn los ultlmos diez alios, se han
utilizado las mediciones de la
susceptibilidad magnetica (MS) de los
sedimentos de los yacimientos
arqueologicos en cueva para
establecer correlaciones entre
yacimientos y una estimacion del
paleoclima. Ello es posible porque la
MS correspondiente a estos
sedimentos es el resultado de los
procesos activos del clima en el
exterior de las cavidades y las
variaciones en las propiedades
magneticas de los sedimentos, que
finalmente se acumulan en el interior
de las cavidades. Una vez que se ban
depositado, estos materiales son
preservados y su estratigraffa
proporciona una informacion sobre el
clima que puede ser inferida. En este
trabajo, al usar la
magnetosusceptibilidad, el metodo de
cicloestratigrafia (MSEC) y la
correlacion grafica, presentamos
informacion sobre la Cova de les
Cendres y situamos estos resultados
en un marco paleoclimatico que
abarca los ultimos 43.000 anos
(fechas BP sin calibrar) de la Europa
meridional. Estos resultados
correlacionan bien con otros
indicadores independientes de clima.
Ademas, a causa de que los
sedimentos de la parte superior de la
Cova de les Cendres se depositaron
relativamente rapidos, es posible
observar cambios climaticos de
escala ultra-fina en los dates de esta
parte de la secuencia en la cavidad.During the last 10 years or so,
magnetic susceptibility (MS)
measurements of cave sediments
from archaeological sites have been
used for intra-site correlation and
paleoclimate estimation. This is
possible because the MS of these
sediments results from climate
processes active outside caves
causing variations in magnetic
properties of the sediments ultimately
accumulating inside of caves. Once
deposited, these materials are
preserved and their stratigraphy
provides a climate proxy that can be
extracted. Here, using the
magnetosusceptibility event and
cyclostratigraphy (MSEC) method and
graphic correlation, we present data
from Cova de les Cendres and place
these results into a paleoclimatic
framework for the last 43,000 years
(uncalibrated BP) for southern
Europe. These results correlate well
with independent climate indicators. In
addition, because sediments in the
upper part of Cova de les Cendres
were deposited relatively quickly, it is
possible to see ultra fine scale
climatic changes in the data set from
this cave.06382<a class="citation_author_name" title="Browse by Author Name for Ellwood, Brooks" href="/fez/list/author/Ellwood, Brooks/">Ellwood, Brooks</a>, <a class="citation_author_name" title="Browse by Author Name for Villaverde Bonilla, Valentín" href="/fez/list/author/Villaverde Bonilla, Valentín/">Villaverde Bonilla, Valentín</a>, <a class="citation_author_name" title="Browse by Author Name for Benoist, Stephen L." href="/fez/list/author/Benoist, Stephen L./">Benoist, Stephen L.</a>, <a class="citation_author_name" title="Browse by Author Name for Bernabeu, Joan" href="/fez/list/author/Bernabeu, Joan/">Bernabeu, Joan</a>, <a class="citation_author_name" title="Browse by Author Name for Harrold, Francis B." href="/fez/list/author/Harrold, Francis B./">Harrold, Francis B.</a> and <a class="citation_author_name" title="Browse by Author Name for Thacker, Paul T." href="/fez/list/author/Thacker, Paul T./">Thacker, Paul T.</a> . (<span class="citation_date">2000</span>) <a class="citation_title" title="Click para ver : A Test of the MSEC Method for Paleoclimate and intersite correlations from Late Pleistocene/Holocene cave sites in southern Europe : results from Cova de les Cendres, SE Spain" href="/fez/view/bibliuned:ETFSerie1-2255AB0C-94DE-3638-B963-46D270E6689A">A Test of the MSEC Method for Paleoclimate and intersite correlations from Late Pleistocene/Holocene cave sites in southern Europe : results from Cova de les Cendres, SE Spain</a>. RecordArtículo de revistaPublishedhttp://udcdata.info/068273HistoriaUniversidad Nacional de Educación a Distancia (España). Facultad de Geografía e HistoriaEllwood, BrooksVillaverde Bonilla, ValentínBenoist, Stephen L.Bernabeu, JoanHarrold, Francis B.Thacker, Paul T.bibliuned:ETFSerie1-2255AB0C-94DE-3638-B963-46D270E6689Ahttp://e-spacio.uned.es/fez/view/bibliuned:ETFSerie1-2255AB0C-94DE-3638-B963-46D270E6689AengDocumento.pdfbibliuned:ETFSerieI2000bibliuned:Setopenairebibliuned:SetarticuloEspacio, tiempo y forma. Serie I, Prehistoria y arqueología. Año 2000, n. 13Set de openaireSet de artículohttp://creativecommons.org/licenses/by-nc-nd/4.0Licencia Creative CommonsEllwoodAcceso abierto3.699456222222222222