Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits
Autor(a) principal: | |
---|---|
Data de Publicação: | 2011 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10451/37886 |
Resumo: | The activity of geomorphic processes in the current periglacial belt of Sierra Nevada during the Holocene has been strongly controlled by climate variability. We examined two sedimentary records showing several cycles with varying intensity of slope processes in the massif. Chronostratigraphic studies of solifluction landforms have revealed seven cycles of enhanced slope activity in Sierra Nevada during the last 7 ka. Lake sediments show eight periods with increased slope activity over the last 6 ka. Depending on temperature and moisture regime, erosion or conditions of slope stability prevailed. Cold and wet periods triggered slope processes and favoured deposition of coarse-grained sediments into the lakes, whereas warm phases were prone to soil development and fine-grained sedimentation in the lakes. The lake sediments also show evidence for an increasing aridity trend since the Holocene Optimum Warm Period in Sierra Nevada, which induced a shift of solifluction processes to higher elevations accompanying late-lying snow patches. |
id |
RCAP_74ea24b26cf210c10ec6615516a9da45 |
---|---|
oai_identifier_str |
oai:repositorio.ul.pt:10451/37886 |
network_acronym_str |
RCAP |
network_name_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository_id_str |
7160 |
spelling |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake depositsHaloceneSedimentological analysisSlope dynamicsLake depositsSierra NevadaSpainThe activity of geomorphic processes in the current periglacial belt of Sierra Nevada during the Holocene has been strongly controlled by climate variability. We examined two sedimentary records showing several cycles with varying intensity of slope processes in the massif. Chronostratigraphic studies of solifluction landforms have revealed seven cycles of enhanced slope activity in Sierra Nevada during the last 7 ka. Lake sediments show eight periods with increased slope activity over the last 6 ka. Depending on temperature and moisture regime, erosion or conditions of slope stability prevailed. Cold and wet periods triggered slope processes and favoured deposition of coarse-grained sediments into the lakes, whereas warm phases were prone to soil development and fine-grained sedimentation in the lakes. The lake sediments also show evidence for an increasing aridity trend since the Holocene Optimum Warm Period in Sierra Nevada, which induced a shift of solifluction processes to higher elevations accompanying late-lying snow patches.The Geological Society of LondonRepositório da Universidade de LisboaOliva, MarcOrtiz, A. Gómez2019-04-08T15:17:53Z20112011-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10451/37886engOliva, M., & Ortiz, A. G. (2011). Holocene slope dynamics in Sierra Nevada (south Spain). Sedimentological analysis of solifluction landforms and lake deposits. Geological Society, London, Special Publications, 354(1), 227-239. Doi: 10.1144/SP354.150305-871910.1144/SP354.15metadata only accessinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-11-08T16:35:17Zoai:repositorio.ul.pt:10451/37886Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T21:51:50.830611Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
title |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
spellingShingle |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits Oliva, Marc Halocene Sedimentological analysis Slope dynamics Lake deposits Sierra Nevada Spain |
title_short |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
title_full |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
title_fullStr |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
title_full_unstemmed |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
title_sort |
Holocene slope dynamics in Sierra Nevada (south Spain): sedimentological analysis of solifluction landforms and lake deposits |
author |
Oliva, Marc |
author_facet |
Oliva, Marc Ortiz, A. Gómez |
author_role |
author |
author2 |
Ortiz, A. Gómez |
author2_role |
author |
dc.contributor.none.fl_str_mv |
Repositório da Universidade de Lisboa |
dc.contributor.author.fl_str_mv |
Oliva, Marc Ortiz, A. Gómez |
dc.subject.por.fl_str_mv |
Halocene Sedimentological analysis Slope dynamics Lake deposits Sierra Nevada Spain |
topic |
Halocene Sedimentological analysis Slope dynamics Lake deposits Sierra Nevada Spain |
description |
The activity of geomorphic processes in the current periglacial belt of Sierra Nevada during the Holocene has been strongly controlled by climate variability. We examined two sedimentary records showing several cycles with varying intensity of slope processes in the massif. Chronostratigraphic studies of solifluction landforms have revealed seven cycles of enhanced slope activity in Sierra Nevada during the last 7 ka. Lake sediments show eight periods with increased slope activity over the last 6 ka. Depending on temperature and moisture regime, erosion or conditions of slope stability prevailed. Cold and wet periods triggered slope processes and favoured deposition of coarse-grained sediments into the lakes, whereas warm phases were prone to soil development and fine-grained sedimentation in the lakes. The lake sediments also show evidence for an increasing aridity trend since the Holocene Optimum Warm Period in Sierra Nevada, which induced a shift of solifluction processes to higher elevations accompanying late-lying snow patches. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011 2011-01-01T00:00:00Z 2019-04-08T15:17:53Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10451/37886 |
url |
http://hdl.handle.net/10451/37886 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Oliva, M., & Ortiz, A. G. (2011). Holocene slope dynamics in Sierra Nevada (south Spain). Sedimentological analysis of solifluction landforms and lake deposits. Geological Society, London, Special Publications, 354(1), 227-239. Doi: 10.1144/SP354.15 0305-8719 10.1144/SP354.15 |
dc.rights.driver.fl_str_mv |
metadata only access info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
metadata only access |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
The Geological Society of London |
publisher.none.fl_str_mv |
The Geological Society of London |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
|
_version_ |
1799134454944366593 |