the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Human and climate-environment interactions in Pyrenean landscapes: a Lateglacial-Holocene multiproxy reconstruction
Abstract. Mountain ecosystems present a complex challenge in disentangling the drivers of their long-term transformation. The subalpine belt of the Pyrenees, once forested, is now characterised by a mosaic of forest patches and open landscapes, and represents a key region in herding practices. However, the relative contributions of climate and human activity in driving its change remain intensely contested. We present a high-resolution, multi-proxy reconstruction of landscape dynamics over the last 25,000 years from the southern Pyrenees. By integrating mammal herbivores, fire regime and vegetation dynamics through sedimentary ancient DNA, pollen and charcoal analyses we aim to compare these proxies and identify the timing and drivers of vegetation change and to distinguish anthropogenic from climatic forces. Our results reveal a multi-phase evolution, with Lateglacial and postglacial forest expansion followed by Mid-Holocene openness, initially triggered by Neoglacial cooling but subsequently maintained by pastoral activities. We find that humans opportunistically exploited this openness from the Mid-Holocene onwards, later transitioning to active landscape management through fires and grazing. This study demonstrates that current Pyrenean landscapes are not a product of either humans or climate, but of their synergy over millennia. Effective conservation strategies must integrate an understanding of this deep ecological history with the emulation of traditional practices to preserve these unique, human-shaped biodiversity hotspots.
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Status: open (until 03 Jul 2026)
- RC1: 'Comment on egusphere-2026-2563', Anonymous Referee #1, 18 Jun 2026 reply
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RC2: 'Comment on egusphere-2026-2563', Anonymous Referee #2, 29 Jun 2026
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This manuscript presents a multi-proxy palaeoecological record from a subalpine lake in the Pyrenean mountains. The authors combine pollen and charcoal analysis with a previously published sedaDNA record to reconstruct vegetation and fire dynamics for the last 12000 years, however their pollen analysis reaches back further. The combination of different proxies and the comparison with existing climate records allows the authors to discuss the different drivers of vegetation change and disentangle the impacts of climate and land use on the vegetation. They propose that cooling during the Neoglacial led to an opening of the vegetation, which was exacerbated by anthropogenic activities. Overall, the data is of high quality, the analyses support their statements, and the manuscript is well prepared. However, I do have some comments, suggestions and questions I would like the authors to address before publication. I have attached a pdf document with my comments.
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This manuscript presents a novel multiproxy palaeoecological record from a high-elevation lake located on the southern slope of the Pyrenees, which combines pollen, charcoal and sedaDNA to reconstruct vegetation changes and their drivers during the Lateglacial and the Holocene. The main novelty is the integration of the previously published sedaDNA dataset with the more "classic" palynological record. The fire regime reconstruction of the local fire regime based on the peak detection analysis adds further value to this study. The combination of datasets allows a novel interpretation of the landscape transformation at high elevation in the Pyrenees during the second half of the Holocene that proposes that human intervention was a major driver but was strongly supported by changing climatic conditions associated with the Neoglacial. I consider that the manuscript is overall well prepared, the data are complete and valuable and the discussion of the results is comprehensive and interesting to a broad audience. However, I also have some comments, suggestions, questions and concerns that the authors may consider before their manuscript is published. I provide them in an annotated pdf version of the manuscript that I attach.