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 highresolution 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, crosscorrelation, 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 cooltemperate forests of Fagus sylvatica under mesomediterranean conditions, with summers ca. 1-2 degrees C warmer than today. Cool and moist calderas may thus become increasingly important for maintaining Mediterranean mesophilous forest species under global warming conditions.

Causes of co-existence of cool-temperate Fagus and warm-loving evergreen Quercus forests in central Italy during the Holocene thermal maximum / Beffa, G.; Gobet, E.; Cosgun, S.; Dotta, R.; Hachler, L.; Morlock, M. A.; Sadori, L.; Schlafli, P.; Schworer, C.; Van Vugt, L.; Vogel, H.; Zander, P. D.; Grosjean, M.; Tinner, W.. - In: FOREST ECOSYSTEMS. - ISSN 2197-5620. - 14:(2025). [10.1016/j.fecs.2025.100345]

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

Sadori L.;
2025

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 highresolution 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, crosscorrelation, 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 cooltemperate forests of Fagus sylvatica under mesomediterranean conditions, with summers ca. 1-2 degrees C warmer than today. Cool and moist calderas may thus become increasingly important for maintaining Mediterranean mesophilous forest species under global warming conditions.
2025
palaeoecology; plant-climate interactions; biodiversity; climate warming; Mediterranean; continuous time series
01 Pubblicazione su rivista::01a Articolo in rivista
Causes of co-existence of cool-temperate Fagus and warm-loving evergreen Quercus forests in central Italy during the Holocene thermal maximum / Beffa, G.; Gobet, E.; Cosgun, S.; Dotta, R.; Hachler, L.; Morlock, M. A.; Sadori, L.; Schlafli, P.; Schworer, C.; Van Vugt, L.; Vogel, H.; Zander, P. D.; Grosjean, M.; Tinner, W.. - In: FOREST ECOSYSTEMS. - ISSN 2197-5620. - 14:(2025). [10.1016/j.fecs.2025.100345]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11573/1766267
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