Predicting the effects of ongoing climate warming on vegetation requires a long-term perspective of past ecosystem dynamics. We therefore analysed the sedimentary record from the mire Gola di Lago (985 m a.s.l.) in southern Switzerland, to better understand the vegetation response to past rapid climate change. We present a high-resolution pollen and plant macrofossil study from the Lateglacial to the Early Holocene (13 400-10 400 cal. a BP), a climatic transition that represents a close analogue to current global warming. The vegetation responses during this time match previously analysed palaeoecological sites south of the Alps. At the end of the Bolling-Allerod interstadial, the site was surrounded by open larch forest. The beginning of t...
Treelines are expected to rise to higher elevations with climate warming; the rate and extent howeve...
The Younger Dryas (YD) climatic reversal (12.86-11.65 cal ky BP), especially the warming initiated a...
A deeper understanding of past vegetation dynamics is required to better assess future vegetation re...
Since the Last Glacial Maximum (LGM; end ca. 19 000 cal BP) central European plant communities have ...
1 The Early Holocene sediment of a lake at tree line (Gouillé Rion, 2343 m a.s.l.) in the Swiss Cent...
International audienceWe reconstruct the vegetational history of the southern side of the Alps at 18...
We reconstruct the vegetational history of the southern side of the Alps at 18,000–10,000 cal yr BP ...
We reconstruct the vegetational history of the southern side of the Alps at 18,000–10,000 cal yr BP ...
In order to infer reactions of treeline and alpine vegetation to climatic change, past vegetation ch...
Quaternary climate variability strongly affected ecosystems and vegetation. Climatic oscillations be...
Oxygen isotope records show a major climatic reversal at 8.2 ka in Greenland and Europe. Annually la...
Both climate change and anthropogenic disturbance affect vegetation composition, but it is difficult...
The North Atlantic region experienced abrupt high-amplitude cooling at the onset of the Younger Drya...
The North Atlantic region experienced abrupt high-amplitude cooling at the onset of the Younger Drya...
The North Atlantic region experienced abrupt high-amplitude cooling at the onset of the Younger Drya...
Treelines are expected to rise to higher elevations with climate warming; the rate and extent howeve...
The Younger Dryas (YD) climatic reversal (12.86-11.65 cal ky BP), especially the warming initiated a...
A deeper understanding of past vegetation dynamics is required to better assess future vegetation re...
Since the Last Glacial Maximum (LGM; end ca. 19 000 cal BP) central European plant communities have ...
1 The Early Holocene sediment of a lake at tree line (Gouillé Rion, 2343 m a.s.l.) in the Swiss Cent...
International audienceWe reconstruct the vegetational history of the southern side of the Alps at 18...
We reconstruct the vegetational history of the southern side of the Alps at 18,000–10,000 cal yr BP ...
We reconstruct the vegetational history of the southern side of the Alps at 18,000–10,000 cal yr BP ...
In order to infer reactions of treeline and alpine vegetation to climatic change, past vegetation ch...
Quaternary climate variability strongly affected ecosystems and vegetation. Climatic oscillations be...
Oxygen isotope records show a major climatic reversal at 8.2 ka in Greenland and Europe. Annually la...
Both climate change and anthropogenic disturbance affect vegetation composition, but it is difficult...
The North Atlantic region experienced abrupt high-amplitude cooling at the onset of the Younger Drya...
The North Atlantic region experienced abrupt high-amplitude cooling at the onset of the Younger Drya...
The North Atlantic region experienced abrupt high-amplitude cooling at the onset of the Younger Drya...
Treelines are expected to rise to higher elevations with climate warming; the rate and extent howeve...
The Younger Dryas (YD) climatic reversal (12.86-11.65 cal ky BP), especially the warming initiated a...
A deeper understanding of past vegetation dynamics is required to better assess future vegetation re...