Causes of co-existence of cool-temperate Fagus and warm-loving evergreen Quercus forests in central Italy during the Holocene thermal maximum

Mediterranean forest communities are particularly diverse but at risk due to their sensitivity to global warming. Understanding the long-term vulnerability of Mediterranean vegetation to climate change is crucial for conservation and management purposes. Studies on past changes of forest communities in response to climate change at ecologically meaningful resolutions (i.e., decadal time scales) are therefore essential, but still very rare. The Holocene thermal maximum (HTM; ca. 10,000–5,000 cal years before the present (BP)) may be used to study species and community responses to warmer conditions than during recent decades. We performed high-resolution multiproxy palaeoecological analyses on sediments from crater Lake Mezzano in central Italy to reconstruct vegetation, diversity, and fire dynamics between 8,450 and 7,050 cal years BP. Ordination, cross-correlation, and species response analyses were used to investigate the response of Mediterranean forest communities to HTM climate warming, human impact, and fire. Vegetational changes prior to 7,450 cal years BP were driven by climate. Fagus sylvatica spread into mixed deciduous oak forests during the Early Holocene in response to declining seasonality (cooler summers and warmer winters). Subsequently, Fagus sylvatica declined and evergreen Quercus ilex expanded after 8,200 cal years BP when the climate became warmer. Although reduced, Fagus sylvatica remained important together with deciduous oaks. The co-existence of Fagus sylvatica and evergreen Quercus forests is extremely rare today. Human impact significantly affected forest vegetation after 7,450 cal years BP, when Neolithic agricultural activities became important, ultimately extirpating these special communities but fostering the overall biodiversity. However, their past occurrence in several central Italian calderas during the HTM suggests that these environments provided habitats that permitted the thriving of cool-temperate forests of Fagus sylvatica under meso-Mediterranean conditions, with summers ca. 1–2 °C warmer than today. Cool and moist calderas may thus become increasingly important for maintaining Mediterranean mesophilous forest species under global warming conditions.

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Journal
Forest Ecosystems
Published
2025-05-14
DOI
https://doi.org/10.1016/j.fecs.2025.100345
Citations
1
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
1.30

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article

Causes of co-existence of cool-temperate Fagus and warm-loving evergreen Quercus forests in central Italy during the Holocene thermal maximum

Sevil Coşgun, Giorgia Beffa, Lieveke van Vugt, Marina A. Morlock et al.
1 citations
Forest Ecosystems
Geology and Paleoclimatology Research
1.30
article

Causes of co-existence of cool-temperate Fagus and warm-loving evergreen Quercus forests in central Italy during the Holocene thermal maximum

Sevil Coşgun, Giorgia Beffa, Lieveke van Vugt, Marina A. Morlock, Paul D. Zander, Willy Tinner, Laura Sadori, Martín Grosjean, Hendrik Vogel, Patrick Schläfli, Luc Hächler, Gobet Erika, Dotta Riccardo, Schwörer Christoph
article en
1 citations

Abstract

Mediterranean forest communities are particularly diverse but at risk due to their sensitivity to global warming. Understanding the long-term vulnerability of Mediterranean vegetation to climate change is crucial for conservation and management purposes. Studies on past changes of forest communities in response to climate change at ecologically meaningful resolutions (i.e., decadal time scales) are therefore essential, but still very rare. The Holocene thermal maximum (HTM; ca. 10,000–5,000 cal years before the present (BP)) may be used to study species and community responses to warmer conditions than during recent decades. We performed high-resolution multiproxy palaeoecological analyses on sediments from crater Lake Mezzano in central Italy to reconstruct vegetation, diversity, and fire dynamics between 8,450 and 7,050 cal years BP. Ordination, cross-correlation, and species response analyses were used to investigate the response of Mediterranean forest communities to HTM climate warming, human impact, and fire. Vegetational changes prior to 7,450 cal years BP were driven by climate. Fagus sylvatica spread into mixed deciduous oak forests during the Early Holocene in response to declining seasonality (cooler summers and warmer winters). Subsequently, Fagus sylvatica declined and evergreen Quercus ilex expanded after 8,200 cal years BP when the climate became warmer. Although reduced, Fagus sylvatica remained important together with deciduous oaks. The co-existence of Fagus sylvatica and evergreen Quercus forests is extremely rare today. Human impact significantly affected forest vegetation after 7,450 cal years BP, when Neolithic agricultural activities became important, ultimately extirpating these special communities but fostering the overall biodiversity. However, their past occurrence in several central Italian calderas during the HTM suggests that these environments provided habitats that permitted the thriving of cool-temperate forests of Fagus sylvatica under meso-Mediterranean conditions, with summers ca. 1–2 °C warmer than today. Cool and moist calderas may thus become increasingly important for maintaining Mediterranean mesophilous forest species under global warming conditions.

Forest EcosystemsVol. 14
University of Bern (CH), Oeschger Centre for Climate Change Research (CH)
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Life in Land
Openalex Percentile: Top 23%
Geology and Paleoclimatology Research
1.30
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