Age structure and climate sensitivity of a high Andean relict forest of Polylepis rodolfo-vasquezii in central Peru

被引:3
|
作者
Ticse-Otarola, Ginette [1 ]
Vidal, Osir D. [1 ]
Andreu-Hayles, Laia [2 ,3 ,4 ]
Quispe-Melgar, Harold R. [5 ,6 ]
Amoroso, Mariano M. [7 ,8 ]
Santos, Guaciara M. [9 ]
Requena-Rojas, Edilson J. [1 ]
机构
[1] Univ Continental, Lab Dendrocronol, Av San Carlos 1980, Huancayo, Peru
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[3] CREAF, Barcelona, Spain
[4] ICREA, Pg Lluis Co 23, Barcelona, Spain
[5] Asociac ANDINUS, Programa Invest Ecol & Biodivers, Calle Miguel Grau 370, Sicaya, Huancayo, Junin, Peru
[6] Univ Continental, Av San Carlos 1980, RA-1980 Huancayo, Junin, Argentina
[7] Univ Nacl Rio Negro, Inst Invest Recursos Nat Agroecol & Desarrollo Rur, Mitre 630, San Carlos De Bariloche, Rio Negro, Argentina
[8] Consejo Nacl Invest Cient & Tecn, Inst Invest Recursos Nat Agroecol & Desarrollo Rur, San Carlos De Bariloche, Rio Negro, Argentina
[9] Univ Calif Irvine, Dept Earth Syst Sci, B321 Croul Hall, Irvine, CA 92697 USA
基金
美国国家科学基金会;
关键词
Conservation; Allometric tree variables; Radiocarbon; Annual periodicity; Forest dynamics; CONSERVATION STATUS; GENUS POLYLEPIS; TREE GROWTH; AUSTRALIS; ALTITUDE; RINGS; RESTORATION; CALIBRATION; COMPETITION; MOUNTAINS;
D O I
10.1016/j.dendro.2023.126071
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
For a better understanding of forest ecology, tree-ring studies can provide information on climate sensitivity, tree growth patterns and population age structure that can inform about stand dynamics such as recruitment of new individuals, and other interspecific interactions related to competition and facilitation. Little is known about the ecology of the recently identified high Andean tree species Polylepis rodolfo-vasquezii. Here, we analyzed the relationship between tree size and age of two P. rodolfo-vasquezii forest stands located in the central Peruvian Andes at 11 degrees S in latitude, and compared their growth patterns and climate sensitivity. We measured the height and diameter of each individual tree and collected tree core samples of living trees and cross sections of dead standing trees to generate two centennial tree-ring chronology at Toldopampa (1825-2015 CE) and at Poma-manta (1824-2014 CE) sites. The dendrochronological dates were evaluated by 14C analysis using the bomb -pulse methods analyzing a total of 9 calendar years that confirm the annual periodicity of this tree species. At the Toldopampa stand most trees ranged from 70 to 80 years old, with a 190-year old individual, being an older and better preserve forest than Pomamanta, with younger trees, probably because more human disturbances due to closer village proximity. No significant relationships were found between tree age and size in the oldest stand alerting that tree diameter should not be used as a metric for estimating tree ages as a general rule. The distinct growth patterns and the size-age relationship observed at the two forests may reflect distinct histories regarding human activities such as fire and logging. Nevertheless, both the Toldopampa and the Pomamanta tree-ring width chronologies exhibited common growth patterns and shared a similar positive response to temperature of the current growing season. Overall, our study confirmed the annual radial growth periodicity in P. rodofolfo-vasquezii trees using an independent method such as 14C analyses and a strong climate sensitivity of this tree species. These findings encourage the development of an extensive P. rodolfo-vasquezii tree-ring network for ecological and paleoclimate studies in the tropical Andes in South America.
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页数:13
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