Climate signal age effects in Pinus uncinata tree-ring density data from the Spanish Pyrenees
Key message The temperature sensitivity of maximum latewood density measurements in pine trees from a highelevation site in the Spanish Pyrenees increases with tree age. Detrending modulates the intensity of the effect. Abstract Tree-rings are the prime archive for high-resolution climate informatio...
| Autores: | , , , , , , , , |
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| Formato: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2025 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:dnet:digitalcsic_::270cc38669650324db1bdee22150bcaa |
| Acesso em linha: | http://hdl.handle.net/10261/428549 |
| Access Level: | acceso abierto |
| Palavra-chave: | Climate change Climate reconstruction Dendrochronology Paleoclimate Tree line |
| Resumo: | Key message The temperature sensitivity of maximum latewood density measurements in pine trees from a highelevation site in the Spanish Pyrenees increases with tree age. Detrending modulates the intensity of the effect. Abstract Tree-rings are the prime archive for high-resolution climate information over the past two millennia. However, the accuracy of annually resolved reconstructions from tree-rings can be constrained by what is known as climate signal age effects (CSAE), encompassing changes in the sensitivity of tree growth to climate over their lifespans. Here, we evaluate CSAE in Pinus uncinata from an upper tree line site in the Spanish central Pyrenees, Lake Gerber, which became a key location for reconstructing western Mediterranean summer temperatures at annual resolution. We use tree-ring width (TRW) and maximum latewood density (MXD) measurements from 50 pine trees with individual ages ranging from 7 to 406 years. For MXD, temperature sensitivity increases significantly (p < 0.01) with tree age from r = 0.31 in juvenile rings with a cambial age < 100 years to r = 0.49 in adult rings > 100 years. Similar CSAE are not detected in TRW, likely affected by the overall lower temperature signal (rTRW = 0.45 vs. rMXD = 0.81 from 1951 to 2020). The severity of CSAE is influenced by the approach used to remove ontogenetic trends, highlighting the need to assess and consider potential biases during tree-ring standardization. Our findings reveal CSAE to add uncertainty in MXD-based climate reconstructions in the Mediterranean. We recommend studying CSAE by sampling diverse age classes in dendroclimatic field campaigns. |
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