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Original title: Holocene klimaatvariabiliteit en ecosysteemveranderingen in de kustzone van Oost en Maritiem Antarctica|
Parent project: Science for a Sustainable Development, more
Reference no: SD/CA/01A
Period: December 2005 till January 2010
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- Universiteit Gent; Laboratorium voor Protistologie en Aquatische Ecologie (PAE), more, co-ordinator
- Universiteit Gent; Faculteit Wetenschappen; Vakgroep Geologie en Bodemkunde; Renard Centre of Marine Geology (RCMG), more, partner
- Université de Liège; Faculté des Sciences; Centre d'Ingénierie des Protéines (CIP), more, partner
- Natural Environment Research Council; British Antarctic Survey (BAS), more, partner
- Belgian Science Policy (BELSPO), more, sponsor
The Earth’s climate undergoes significant changes, which are not yet fully understood. Although the Holocene has not experienced climate changes of the same magnitude as during the major Quaternary glaciations, it has been marked by many, often rapid, global temperature and precipitation anomalies. Recently, parts of the Antarctic Peninsula (AP) region have experienced some of the most rapid warming on Earth, whereas a decline in the temperature record was observed in other Antarctic areas. This temperature rise near the AP has already led to ice shelf disintegration and rapid glacier retreat and influenced marine and terrestrial ecosystems. In order to understand how Antarctic temperature variation in inland and coastal areas are interrelated and can impact other regions on Earth, it is necessary to learn from the record of past natural climate variability.
The IGBP project PAGES (www.pages.unibe.ch) has set up the PEP (Pole-Equator-Pole) traverses 1, 2 and 3 in order to determine past climate changes along continental transects. HOLANT will explicitly extend the PEP 1 transect towards Sub-Antarctica and coastal Maritime Antarctica and contribute to the PEP2 and 3 transects by establishing and comparing a series of high resolution records of Holocene climate variability in coastal Antarctica based upon biological and sedimentological proxies in (coastal) lake sediments.
The specific research questions are:
- What are the timing, duration and magnitude of Holocene climate anomalies in coastal areas in maritime and east Antarctic regions and how are these anomalies related to climatic events recorded in inland locations (ice cores)?
- How did Holocene climate changes affect regional ice sheet/glacier dynamics?
- How did Holocene climate changes affect the diversity of primary producers in Antarctic lakes?
HOLANT will use biological and sedimentological proxies and seismic surveys to reconstruct past climate changes and the evolution of climatically influenced lake basins in coastal Antarctic and Sub-Antarctic regions. In parallel, we will exploit our newly-developed techniques to study fossil DNA in lake sediments as a tool to reveal the response of the basal food web to past climate anomalies. We will relate the emerging spatio-temporal pattern in climate changes in Antarctica to changes in regional ice sheet volume and to global-scale climate anomalies during the past 10,000 years.
Interactions between the different partners
The scientific activities are organised into seven work packages (WP). The responsible partner is indicated after each task/work package.
WP1: Field work
- Task 1.1. Coring and sampling of lakes in Maritime Antarctica (BAS, PAE)
- Task 1.2. Coring, sampling and seismic survey of lakes near Syowa Oasis (PAE, BAS, RCMG)
- Task 1.3. Coring, sampling and seismic survey of lakes on Kerguelen Archipelago (RCMG)
WP 2: Establishment of sediment chronology from cores (BAS, PAE)
WP 3: Reconstruction of past climate changes using sedimentological and biological proxies in lake-sediment cores
- Task 3.1. Sedimentological parameters as indicators of past changes in the main sediment input processes of the lake (RCMG)
- Task 3.2. Diatoms as indicators of past changes in productivity and in the precipitation-evaporation balance (PAE)
- Task 3.3. Reconstruction of changes in lake productivity using fossil pigments, the macrofossil record and loss on ignition (BAS, PAE)
WP 4: development of relative sea-level (RSL) curves and reconstruction of the deglaciation history (BAS, PAE)
WP 5: fossil DNA to reveal the response of the basal food web to past climate anomalies (CIP, PAE)
WP 6: reconstruction of regional climate change and i