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Climatic response of Juniperus monticola Martinez, a multi-century alpine shrub from the high mountains of central Mexico

Bibliographic Data

ID7170435
AuthorsLorenzo Vázquez-Selem (0000-0001-7798-6187, Instituto de Geografía, Universidad Nacional Autónoma de México, Ciudad Universitaria, México), Osvaldo Franco-Ramos (Instituto de Geografía, Universidad Nacional Autónoma de México, Ciudad Universitaria, México), Osvaldo Franco‐Ramos (0000-0001-9261-5755, Universidad Nacional Autonoma de Mexico), José Villanueva-Díaz (0000-0001-8211-1203, Laboratorio de Dendrocronología, Instituto Nacional de Investigaciones Forestales, Agrícolas, y Pecuarias, CENID-RESPID, Mexico, corresponding author), Julián Cerano‐Paredes (0000-0002-1528-5139, Instituto Nacional de Investigaciones Forestales Agrícolas y Pecuarias), Julián Cerano-Paredes (Laboratorio de Dendrocronología, Instituto Nacional de Investigaciones Forestales, Agrícolas, y Pecuarias, CENID-RESPID, Mexico), David W Stahle (Tree-Ring Laboratory, Department of Geosciences, University of Arkansas, USA)
Year2025
Volume35
Issue1
Pages100-110
Publication date2025-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publications Inc (PUBLISHER)
DOI10.1177/09596836241286006
OpenAlexW4402898660
LanguageEN
References cited61

The mountain juniper Juniperus monticola Martinez, a decumbent alpine shrub found at elevations up to 4600 m a.s.l. on the high mountains of central Mexico, is the woody species growing at highest elevation in North America. It reaches an age close to a millenium, which probably makes it the oldest alpine shrub in the world. We conducted a dendrochronological study of this species at Pico de Orizaba volcano, the highest peak in Mexico, to analyze its dendroclimatic potential and the influence of ocean-atmospheric forcing on the interannual variability of radial growth. A ring-width chronology was developed extending from 1178 to 2016 (839 years). Climate data from a local weather station and from CRU TS version 4.01 were used to determine the climatic response of J. monticola . The species is positively correlated to the average maximum temperature of May–June ( r = 0.38, p r = −0.44, p r = −0.354, p r = −0.4, p

Biology · Chronology · Climate change · Climatology · Dendroclimatology · Evapotranspiration · Geography · Juniper · Meteorology · Physical geography · Precipitation · Shrub · Climate variability and models · Environmental Science · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses · Ecology · Forestry · Geology

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Citation velocityhistorical
Highly citedNo
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