A 12,700-year history of paleolimnological change from an Andean microrefugium

We present a 12,6700-yr limnological history of Lake Miski, a high-elevation lake in a wet section of the Peruvian Andes. While many shallow Andean lakes dried up during the mid-Holocene, loss-on-ignition, magnetic susceptibility, and diatom analysis showed that Lake Miski was a constant feature in...

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Main Author: de Novaes Nascimento, Majoi (author)
Other Authors: Laurenzi, Anne Gail (author), Valencia, Bryan G. (author), Van, Robert (author), Bush, Mark (author)
Format: article
Published: 2018
Subjects:
Online Access:http://repositorio.ikiam.edu.ec/jspui/handle/RD_IKIAM/78
https://doi.org/10.1177/0959683618810400
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author de Novaes Nascimento, Majoi
author2 Laurenzi, Anne Gail
Valencia, Bryan G.
Van, Robert
Bush, Mark
author2_role author
author
author
author
author_facet de Novaes Nascimento, Majoi
Laurenzi, Anne Gail
Valencia, Bryan G.
Van, Robert
Bush, Mark
author_role author
collection Repositorio Universidad Regional Amazónica
dc.creator.none.fl_str_mv de Novaes Nascimento, Majoi
Laurenzi, Anne Gail
Valencia, Bryan G.
Van, Robert
Bush, Mark
dc.date.none.fl_str_mv 2018
2019-05-15T21:08:13Z
2019-05-15T21:08:13Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv de Novaes Nascimento, M., Laurenzi, A. G., Valencia, B. G., Van, R., & Bush, M. (2019). A 12,700-year history of paleolimnological change from an Andean microrefugium. Holocene, 29(2), 231–243. doi.org/10.1177/0959683618810400
doi.org/10.1177/0959683618810400
http://repositorio.ikiam.edu.ec/jspui/handle/RD_IKIAM/78
https://doi.org/10.1177/0959683618810400
dc.language.none.fl_str_mv en
dc.publisher.none.fl_str_mv SAGE Publications
dc.relation.none.fl_str_mv PRODUCCION CIENTÍFICA-ARTÍCULOS;A-IKIAM-000021
dc.rights.none.fl_str_mv Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América
http://creativecommons.org/licenses/by-nc-nd/3.0/us/
info:eu-repo/semantics/openAccess
dc.source.none.fl_str_mv reponame:Repositorio Universidad Regional Amazónica
instname:Universidad Regional Amazónica
instacron:IKIAM
dc.subject.none.fl_str_mv Andes
Diatoms
Limnology
Microrefugia
Paleocology
Drought
Holocene
ENSO
Mid-Holocene dry event
dc.title.none.fl_str_mv A 12,700-year history of paleolimnological change from an Andean microrefugium
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/article
description We present a 12,6700-yr limnological history of Lake Miski, a high-elevation lake in a wet section of the Peruvian Andes. While many shallow Andean lakes dried up during the mid-Holocene, loss-on-ignition, magnetic susceptibility, and diatom analysis showed that Lake Miski was a constant feature in the landscape. Overall, fluctuations in the fossil diatom communities of Lake Miski tracked changes in insolation, but this was not the only mechanism influencing observed variability. We identify periods when insolation and interactions with the Pacific Ocean may have played a role in structuring local climate and diatom assemblages. The true mid-Holocene Dry Event (MHDE) is manifested in this record between 8000 and 5000 cal BP, but the carbonate stratigraphy and the diatom community indicated that although the level of the lake decreased, it never completely dried out, instead there was higher availability of planktic habitat and stronger mixing than in much of the Holocene. High rates of biological change observed during the late-Holocene in other records from Peru associated with human amplification of climatic signals were not observed in Lake Miski, as this lake may have been too wet and remote to be strongly influenced by human activity. Because of the presence of a woodland microrefugium, Lake Miski was suggested to have been an unusually climatically stable and wet location during the regional drying associated with the MHDE. Our new limnological information provides additional insights relating to this discussion. The presence of the observed woodland apparently withstood fluctuations that induced state changes in the lake and diatom flora, underscoring that microrefugia do not equate to ‘unchanging’ hydrologies or climates
eu_rights_str_mv openAccess
format article
id IKIAM_70350b978cdf5d28cf3f9fa93a67c7c2
identifier_str_mv de Novaes Nascimento, M., Laurenzi, A. G., Valencia, B. G., Van, R., & Bush, M. (2019). A 12,700-year history of paleolimnological change from an Andean microrefugium. Holocene, 29(2), 231–243. doi.org/10.1177/0959683618810400
doi.org/10.1177/0959683618810400
instacron_str IKIAM
institution IKIAM
instname_str Universidad Regional Amazónica
language_invalid_str_mv en
network_acronym_str IKIAM
network_name_str Repositorio Universidad Regional Amazónica
oai_identifier_str oai:repositorio.ikiam.edu.ec:RD_IKIAM/78
publishDate 2018
publisher.none.fl_str_mv SAGE Publications
reponame_str Repositorio Universidad Regional Amazónica
repository.mail.fl_str_mv .
repository.name.fl_str_mv Repositorio Universidad Regional Amazónica - Universidad Regional Amazónica
repository_id_str 0
rights_invalid_str_mv Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América
http://creativecommons.org/licenses/by-nc-nd/3.0/us/
spelling A 12,700-year history of paleolimnological change from an Andean microrefugiumde Novaes Nascimento, MajoiLaurenzi, Anne GailValencia, Bryan G.Van, RobertBush, MarkAndesDiatomsLimnologyMicrorefugiaPaleocologyDroughtHoloceneENSOMid-Holocene dry eventWe present a 12,6700-yr limnological history of Lake Miski, a high-elevation lake in a wet section of the Peruvian Andes. While many shallow Andean lakes dried up during the mid-Holocene, loss-on-ignition, magnetic susceptibility, and diatom analysis showed that Lake Miski was a constant feature in the landscape. Overall, fluctuations in the fossil diatom communities of Lake Miski tracked changes in insolation, but this was not the only mechanism influencing observed variability. We identify periods when insolation and interactions with the Pacific Ocean may have played a role in structuring local climate and diatom assemblages. The true mid-Holocene Dry Event (MHDE) is manifested in this record between 8000 and 5000 cal BP, but the carbonate stratigraphy and the diatom community indicated that although the level of the lake decreased, it never completely dried out, instead there was higher availability of planktic habitat and stronger mixing than in much of the Holocene. High rates of biological change observed during the late-Holocene in other records from Peru associated with human amplification of climatic signals were not observed in Lake Miski, as this lake may have been too wet and remote to be strongly influenced by human activity. Because of the presence of a woodland microrefugium, Lake Miski was suggested to have been an unusually climatically stable and wet location during the regional drying associated with the MHDE. Our new limnological information provides additional insights relating to this discussion. The presence of the observed woodland apparently withstood fluctuations that induced state changes in the lake and diatom flora, underscoring that microrefugia do not equate to ‘unchanging’ hydrologies or climatesSCIMAGO JOURNAL RANKSAGE Publications2019-05-15T21:08:13Z2019-05-15T21:08:13Z2018info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfde Novaes Nascimento, M., Laurenzi, A. G., Valencia, B. G., Van, R., & Bush, M. (2019). A 12,700-year history of paleolimnological change from an Andean microrefugium. Holocene, 29(2), 231–243. doi.org/10.1177/0959683618810400doi.org/10.1177/0959683618810400http://repositorio.ikiam.edu.ec/jspui/handle/RD_IKIAM/78https://doi.org/10.1177/0959683618810400enPRODUCCION CIENTÍFICA-ARTÍCULOS;A-IKIAM-000021Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de Américahttp://creativecommons.org/licenses/by-nc-nd/3.0/us/info:eu-repo/semantics/openAccessreponame:Repositorio Universidad Regional Amazónicainstname:Universidad Regional Amazónicainstacron:IKIAM2023-08-08T20:06:32Zoai:repositorio.ikiam.edu.ec:RD_IKIAM/78Institucionalhttps://repositorio.ikiam.edu.ec/Universidad públicahttps://www.ikiam.edu.ec/https://repositorio.ikiam.edu.ec/oaiEcuador...opendoar:02023-08-08T20:06:32falseInstitucionalhttps://repositorio.ikiam.edu.ec/Universidad públicahttps://www.ikiam.edu.ec/https://repositorio.ikiam.edu.ec/oai.Ecuador...opendoar:02023-08-08T20:06:32Repositorio Universidad Regional Amazónica - Universidad Regional Amazónicafalse
spellingShingle A 12,700-year history of paleolimnological change from an Andean microrefugium
de Novaes Nascimento, Majoi
Andes
Diatoms
Limnology
Microrefugia
Paleocology
Drought
Holocene
ENSO
Mid-Holocene dry event
status_str publishedVersion
title A 12,700-year history of paleolimnological change from an Andean microrefugium
title_full A 12,700-year history of paleolimnological change from an Andean microrefugium
title_fullStr A 12,700-year history of paleolimnological change from an Andean microrefugium
title_full_unstemmed A 12,700-year history of paleolimnological change from an Andean microrefugium
title_short A 12,700-year history of paleolimnological change from an Andean microrefugium
title_sort A 12,700-year history of paleolimnological change from an Andean microrefugium
topic Andes
Diatoms
Limnology
Microrefugia
Paleocology
Drought
Holocene
ENSO
Mid-Holocene dry event
url http://repositorio.ikiam.edu.ec/jspui/handle/RD_IKIAM/78
https://doi.org/10.1177/0959683618810400