Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico

A climate-sensitive ring-width chronology of the endemic Guadalupe cypress (Hesperocyparis guadalupensis) was developed for the Guadalupe Island. The chronology length covers the last 205 years (1804-2008) and was significantly correlated (r = 0.45 a 0.48, p<0.000) with ring-width chronologie...

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Hoofdauteurs: Villanueva Díaz, José, Cerano Paredes, Julián, Olivares Bañuelos, Nadia C., Valles Pérez, Miguel, Stahle, David W., Cervantes Martínez, Rosalinda
Formaat: Online
Taal:spa
Gepubliceerd in: Instituto de Ecología, A.C. 2015
Online toegang:https://myb.ojs.inecol.mx/index.php/myb/article/view/464
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author Villanueva Díaz, José
Cerano Paredes, Julián
Olivares Bañuelos, Nadia C.
Valles Pérez, Miguel
Stahle, David W.
Cervantes Martínez, Rosalinda
author_facet Villanueva Díaz, José
Cerano Paredes, Julián
Olivares Bañuelos, Nadia C.
Valles Pérez, Miguel
Stahle, David W.
Cervantes Martínez, Rosalinda
author_sort Villanueva Díaz, José
collection MYB
description A climate-sensitive ring-width chronology of the endemic Guadalupe cypress (Hesperocyparis guadalupensis) was developed for the Guadalupe Island. The chronology length covers the last 205 years (1804-2008) and was significantly correlated (r = 0.45 a 0.48, p<0.000) with ring-width chronologies from the areas of Baja California, California, and southern Canada formerly used to analyze the influence and for reconstruction purposes of the PDO. This association was weak and non-significant with chronologies developed along the western slopes of the Sierra Madre Occidental, probably influenced by other circulatory patterns. The cypress chronology showed a significant association with instrumental (r= 0.414, P<0.000, n = 109) and reconstructed (r= 0.68 p<0.000, n= 109) indices of the PDO. The chronology was significantly associated (r= 0.65, p<0.0005, n= 44) with the January-November precipitation for weather stations in Ensenada indicating potential for climate reconstructions. The spectral analysis of the ring-width chronology detected significant peaks at frequencies from 12 to 28 years and 50 to 70 years which are associated to the PDO effect, and peaks of 6.8 more related to the ENSO effect. The location of the chronology at the southern extreme of the PDO influence area may be important to analyze in greater detail the impact of the PDO and other atmospheric phenomena such as ENSO. The observed climatic response of cypress opens new research opportunities for paleoclimatic studies and may be useful to plan for restoration and conservation actions of this and other associated species.
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spelling oai:oai.myb.ojs.inecol.mx:article-4642022-11-30T05:46:03Z Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico Respuesta climática del ciprés (Hesperocyparis guadalupensis) en Isla Guadalupe, Baja California, México Villanueva Díaz, José Cerano Paredes, Julián Olivares Bañuelos, Nadia C. Valles Pérez, Miguel Stahle, David W. Cervantes Martínez, Rosalinda Guadalupe cypress dendrochronology ENSO frequencies PDO droughts ciprés de Guadalupe dendrocronología ENSO frecuencias PDO sequías A climate-sensitive ring-width chronology of the endemic Guadalupe cypress (Hesperocyparis guadalupensis) was developed for the Guadalupe Island. The chronology length covers the last 205 years (1804-2008) and was significantly correlated (r = 0.45 a 0.48, p<0.000) with ring-width chronologies from the areas of Baja California, California, and southern Canada formerly used to analyze the influence and for reconstruction purposes of the PDO. This association was weak and non-significant with chronologies developed along the western slopes of the Sierra Madre Occidental, probably influenced by other circulatory patterns. The cypress chronology showed a significant association with instrumental (r= 0.414, P<0.000, n = 109) and reconstructed (r= 0.68 p<0.000, n= 109) indices of the PDO. The chronology was significantly associated (r= 0.65, p<0.0005, n= 44) with the January-November precipitation for weather stations in Ensenada indicating potential for climate reconstructions. The spectral analysis of the ring-width chronology detected significant peaks at frequencies from 12 to 28 years and 50 to 70 years which are associated to the PDO effect, and peaks of 6.8 more related to the ENSO effect. The location of the chronology at the southern extreme of the PDO influence area may be important to analyze in greater detail the impact of the PDO and other atmospheric phenomena such as ENSO. The observed climatic response of cypress opens new research opportunities for paleoclimatic studies and may be useful to plan for restoration and conservation actions of this and other associated species. Una serie dendrocronológica climáticamente sensitiva de anillo total se desarrolló en Isla Guadalupe con la especie endémica ciprés de Guadalupe (Hesperocyparis guadalupensis (S. Watson) Bartel. Var. guadalupensis). La cronología comprende los últimos 205 años (1804-2008) y mostró una respuesta significativa (r = 0.45 a 0.48, p<0.0001) con cronologías de anillos de árboles procedentes de Baja California, California y Sur de Canadá, utilizadas para análisis del impacto y reconstrucción del PDO. No obstante, esta asociación fue débil con cronologías desarrolladas en la Sierra Madre Occidental, que probablemente estén influenciadas por otros fenómenos circulatorios. Se encontró una respuesta significativa con registros instrumentales (r= 0.414, p<0.0001, n = 109) y reconstruidos (r= 0.68 p<0.0001, n= 109) del PDO. La cronología se asoció significativamente con la lluvia enero-noviembre de Ensenada (r= 0.65, p<0.0005, n= 44), indicando potencial para reconstrucciones de clima. El análisis espectral de la serie dendrocronológica detectó la presencia de frecuencias significativas de 12 años a 28 años y de 50 años a 70 años, que se relacionan con el PDO; mientras que la frecuencia significativa de 6.8 años pudiera estar relacionada con ENSO. Dado que la cronología se ubica en el extremo más al sur de la influencia del PDO, esta puede ser de utilidad para determinar el área de influencia de este fenómeno y el posible impacto de otros como ENSO. La respuesta climática encontrada con esta especie, abre oportunidades para nuevas investigaciones paleoclimáticas, que a la vez son importantes para promover acciones de restauración de ecosistemas y la conservación de esta y de otras especies asociadas. Instituto de Ecología, A.C. 2015-12-11 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Artículo evaluado por pares application/pdf text/html https://myb.ojs.inecol.mx/index.php/myb/article/view/464 10.21829/myb.2015.213464 Madera y Bosques; Vol. 21 No. 3 (2015): Otoño Madera y Bosques; Vol. 21 Núm. 3 (2015): Otoño 2448-7597 1405-0471 spa https://myb.ojs.inecol.mx/index.php/myb/article/view/464/630 https://myb.ojs.inecol.mx/index.php/myb/article/view/464/645 Derechos de autor 2016 Madera y Bosques
spellingShingle Villanueva Díaz, José
Cerano Paredes, Julián
Olivares Bañuelos, Nadia C.
Valles Pérez, Miguel
Stahle, David W.
Cervantes Martínez, Rosalinda
Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico
title Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico
title_full Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico
title_fullStr Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico
title_full_unstemmed Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico
title_short Climatic response of Guadalupe cypress (Hesperocyparis guadalupensis) in Guadalupe island, Baja California, Mexico
title_sort climatic response of guadalupe cypress (hesperocyparis guadalupensis) in guadalupe island, baja california, mexico
url https://myb.ojs.inecol.mx/index.php/myb/article/view/464
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