TY - CONF
T1 - Impact of Climate events over the Last Glacial-Interglacial Transition
AU - Hoek, Wim
AU - Birks, Hilary
AU - WG4Members, Intimate
PY - 2013/4/1
Y1 - 2013/4/1
N2 - The time period from 60-8 ka cal BP is marked by a series of abrupt
climate events that became apparent from especially the Greenland Ice
core records. These ice core records furthermore provided a precise and
detailed chronology for the occurrence of these climate events. In the
European terrestrial environment numerous studies have shown that these
climate events have had an impact on the environment, ranging from
geomorphological changes, changes in vegetation composition, faunal
composition, and human behaviour and development. However, the
recognition of the impact of the different events is strongly dependent
on reliable age models for the environmental records. This requires a
careful selection and analysis of existing data. Working Group 4 of
the INTIMATE COST action aims to review the nature and quality of
climate reconstructions of past environmental change across the full
range of European environments (Mediterranean to sub-Arctic). For this
we try to enlarge the European network of researchers, stimulate data
sharing and eventually synthesise thematic environmental datasets.
Important aspects are to identify the impacts of abrupt and extreme
change and reveal the timing, duration and thresholds of climate impact.
The first results for selected climate events show that clear gradients
and thresholds exist, especially in ecotonal environmental settings.
Resilience and inertia of the ecosystem and its components will
determine whether thresholds are crossed or not and whether changes are
so large that they could be considered as a regime shift (for example
the change from tundra or steppe to forest). Environmental and
particularly biotic responses will always lag the climate driver by very
small to considerable amounts of time, depending on the biological
traits and distributions of the organisms concerned. Therefore, we
should not expect the apparent consequences of climate-driven changes to
be synchronous across the European continent. We aim to identify
sensitive areas for study from where we will obtain the most useful
information about the impacts of climate changes.
AB - The time period from 60-8 ka cal BP is marked by a series of abrupt
climate events that became apparent from especially the Greenland Ice
core records. These ice core records furthermore provided a precise and
detailed chronology for the occurrence of these climate events. In the
European terrestrial environment numerous studies have shown that these
climate events have had an impact on the environment, ranging from
geomorphological changes, changes in vegetation composition, faunal
composition, and human behaviour and development. However, the
recognition of the impact of the different events is strongly dependent
on reliable age models for the environmental records. This requires a
careful selection and analysis of existing data. Working Group 4 of
the INTIMATE COST action aims to review the nature and quality of
climate reconstructions of past environmental change across the full
range of European environments (Mediterranean to sub-Arctic). For this
we try to enlarge the European network of researchers, stimulate data
sharing and eventually synthesise thematic environmental datasets.
Important aspects are to identify the impacts of abrupt and extreme
change and reveal the timing, duration and thresholds of climate impact.
The first results for selected climate events show that clear gradients
and thresholds exist, especially in ecotonal environmental settings.
Resilience and inertia of the ecosystem and its components will
determine whether thresholds are crossed or not and whether changes are
so large that they could be considered as a regime shift (for example
the change from tundra or steppe to forest). Environmental and
particularly biotic responses will always lag the climate driver by very
small to considerable amounts of time, depending on the biological
traits and distributions of the organisms concerned. Therefore, we
should not expect the apparent consequences of climate-driven changes to
be synchronous across the European continent. We aim to identify
sensitive areas for study from where we will obtain the most useful
information about the impacts of climate changes.
M3 - Poster
SP - 12929
ER -