Südchina, insbes. die Provinz Guandong, ist eines der am dichtesten besiedelten Gebiete der Erde. Positive Konsequenz dieser Ballung ist eine äußerst dynamische Wirtschaftsentwicklung, aber gerade diese von subtropischem Monsunklima geprägte Region ist auch immer wieder Ausgangspunkt für sich schnell und zunehmend global ausbreitende epidemische Krankheiten wie zuletzt SARS. Mit der globalen Erwärmung einhergehende Klimaveränderungen könnten sich für diese Region insbesondere durch Veränderungen der Häufigkeit und Intensität tropischer Wirbelstürme, aber auch Änderungen der Niederschlagsmenge- und Intensität bemerkbar machen. Im Gegensatz zu den schon recht umfangreichen Datensätzen aus der Südchinesischen See (SCS) gibt es bisher jedoch nur sehr wenige terrestrische Paläoklimaarchive aus der Region, die Klimaveränderungen während des Holozäns, des Spätglazials oder Glazials hochauflösend dokumentieren. Wir haben deshalb einen an der nördlichen Küste der SCS gelegenen Maarsee ausgewählt, um über die Analyse von Proxydaten aus Seesedimenten solche Paläo-Klimavariationen zu untersuchen. Aus dem Sediment des Huguang-Maarsees wurden mittels Usinger-Präzisionsstechtechnik von einem Floss aus insgesamt 7 Sedimentsequenzen gewonnen, von denen die tiefste bis 57 m unter den Seeboden reicht. Die zeitliche Einstufung der Profile wurde mit Hilfe von 17 Radiokohlenstoff-Datierungen vorgenommen und ergab ein extrapoliertes Maximalalter von ca. 78.000 Jahren. Ein breites Spektrum aus sedimentologischen, geochemischen, paläo- und gesteinsmagnetischen sowie palynologischen Methoden kam sodann zum Einsatz, um die Paläo-Umweltbedingungen, die natürlich immer das entsprechende Klima widerspiegeln, während dieses Zeitraumes zu rekonstruieren. Überraschenderweise ergab sich ein von vielen bekannten Klimaprofilen der Nordhemisphäre (insbes. des Atlantikraumes, aber auch mariner Kerne aus dem Indik und Südostasien) abweichendes Muster. Im Gegensatz zu dem bekannten Grundmuster eines vergleichsweise stabilen Klimas während des Holozäns und stärkerer Schwankungen während des letzten Glazials weisen die Daten aus dem Huguang-Maarsee für das letzte Glazial im Zeitraum zwischen 15.000 und 40.000 Jahren auf relativ stabile Umweltbedingungen hin. Die älteren Bereiche zwischen 40.000 und ca. 78.000 Jahren haben durch Eintrag von umgelagertem Torf eine eher lokale Komponente und sind somit für den regionalen und globalen Vergleich ungeeignet. Das Holozän hingegen zeichnet sich durch hohe Schwankungsamplituden vieler Proxydaten (Karbonatgehalt, magnetische Suszeptibilität, organischer Kohlenstoff, Trockendichte, gesteinsmagnetische Parameter, Redox-Verhältnisse) aus, die auf ein recht variables Klima hinweisen. Besonders interessant ist die Übergangsphase vom Glazial zum Holozän, die bei etwa 15.000 Jahren vor heute in etwa zeitgleich mit dem beobachteten stärksten Meeresspiegelanstieg der Südchinesischen See einsetzt und eine abrupte Intensitätszunahme des Sommermonsuns anzeigt
The physiological fundamentals of temperature dependent distribution limits in cold oceans are addressed as a precondition to understand ecological performance and ecosystem function. The study will focus on the specific role of extracellular ion concentration in setting limitations to lifestyle and life history evolution. The biogeography of marine crustaceans in cold oceans is related to the combined effects of extracellular Mg2+ levels (Mg2+)e and low temperature, which act synergistically to slow muscular activity in the cold. The highly active cephalopod molluscs may have overcome the constraint of high (Mg2+)e by slightly increasing the extracellular potassium concentration ((K+)e), thereby exploiting the antagonistic effects of magnesium and potassium. We attempt to develop quantitative knowledge of the temperature dependent effects of potassium and magnesium on animal life cycle resulting from changes in physiology performance, larval development, and growth rate. In addition, it appears most crucial to understand the biochemical mechanisms leading to the increased magnesium effect in the cold. Within the crustacean phyla this work will focus on the lithodid crabs. They are suitable for such studies since they have a wide distribution range north and south of the Antarctic convergence and thus covering a broad temperature regime. For comparable studies boreal reptant crabs and boreal and Antarctic natant shrimps will also be included. Within the cephalopod phyla we will concentrate on the boreal species Sepia officinalis to investigate principle mechanisms. Accordingly, the present study is intended to explore, from a more conceptual point of view, whether limitations in ion regulation capacities and costs may play a role in setting the levels of biodiversity observed in extant Antarctic marine fauna.
In the framework of the international ANtarctic DRILLing program (ANDRILL) the 1138 m deep core borehole SMS was drilled in the Southern McMurdo Sound (Ross Sea). The investigations of Antarctic Neogene ice sheet variations, of long-term climate evolutions and of the tectonic history of McMurdo Sound represent the main project aims. One part of the German participation in the ANDRILL project is the extensive geophysical logging of the SMS borehole. It delivers a main basis for answering a lot of questions in the scope of the whole project consisting of about 100 scientists. Interpreting the downhole logging data permits among other things to establish a complete lithological log, to characterize the drilled sediments petrophysically, to determine sedimentary structures and to get evidence about palaeoclimatic conditions during up to 19 Mio years. Seismic experiments in the borehole allow linking detailed geological information with shipborne seismic sections. This way, local results can be transformed into spatial information thus providing an important contribution to the understanding of the tectonic structure of the Ross Sea.
The ZEF research focuses on the Tungabhadra basin in south India, which is one of the four basins studied in the project. Tungabhadra river is a tributary of the Krishna river. ZEF will be mainly active in Work Package (WP) 9 IWRM in the twinned Tungabhadra and Tejo/Tagus river basins, with a focus and land and water use interactions . The research focuses on the interaction between irrigated and rainfed farming in the lower Tungabhadra basin, in the border area of the states of Karnataka and Andhra Pradesh. The districts on the Karnataka side are Raichur, Koppal and Bellary, on the Andhra Pradesh side Mahbubnagar and Kurnool. Some of the sub-themes ZEF will look at, together with other partners, are: 1) Flows and relations (people (livelihood linkages, labour), nutrients and energy, money/income, water); 2) Institutional and policy (dis)integration (departmental coordination, agency coordination, policy contradictions and alignments); 3) Innovations (water saving farming systems (SRI and other), (tiered) water users associations, water pricing and water rights, substitutability of technical and institutional solutions to water problems); 4) History (heads and tails of different kinds: the spatial dimension of social differentiation; evolution of policy regimes, natural resources degradation/conservation in historical perspective, land and water use change over time and its implications). It is part of the research design to compare the situation in the Tungabhadra basin with that in the Tajo/Tegus basin in Spain/Portugal. Other basins studied in the larger project are the Glomma basin in Norway and the Sesan basin in Vietnam/Cambodia).
We are proposing an SSA 'SEARCH for DAMOCLES' that is based on recent initiatives started in Europe and the USA in the field of Arctic marine ecosystems and Global change, with specific emphasis on Arctic Ocean long-term observatories. The SSA will capitalize on opportunities and significant benefits arising from coordination of large scale research programmes such as the European Integrated Project DAMOCLES (Developing Arctic Modelling and Observing Capabilities for Long-term Environmental studies) and the US research program SEARCH (Study of Environmental ARctic Change). 'SEARCH for DAMOCLES', positioned in the domain of Arctic Science, will be particularly timely in the context of the International Polar Year and will significantly contribute to the coordinated implementation of the DAMOCLES and SEARCH work programmes in the field of Global Change and Ecosystems. Close synchronization of these programmes will enhance the acquisition of pan-arctic data sets, and their analysis, the dissemination and archiving of results, as well as heightening public awareness. International workshops and conferences including other partners such as Canada, Russia, and Asian countries (Japan, China, and South Korea), will enable translation of the results into planning of integrated, future activities that will be based on the SSA 'SEARCH for DAMOCLES'. The coordination and synchronization of Arctic programs such as DAMOCLES and SEARCH, through an SSA is a unique opportunity to ensure the necessary pan-arctic coverage of observations and data evaluation for understanding Arctic system variability, avoiding major gaps and unnecessary overlaps. This EU-US SSA will also contribute to promotion and facilitation of future RTD activities via prospective studies, exploratory measures and pilot actions. The EU-US SSA 'SEARCH for DAMOCLES' is proposed for 3 years covering the 3 last years of the 4-year DAMOCLES Integrated Project (2006-2009) and the 2 years of the IPY (2007-2008). Prime Contactor: Universite Pierre et Marie Curie - Paris VI; Paris; France.
All EU Member States face economic and ecological losses due to forest damages. Thus, combating forest dieback, as for example caused by climate change, is a contribution to human safety and well-being and the sustainable development of Europe. The Feasibility Study on means of combating forest dieback in the European Union was initiated by the European Parliament demanding the European Commission to develop a concrete proposal for preventing, mitigating and control forest dieback in the EU. The study was carried out by the Institute for World Forestry and the European Forest Institute (EFI) in 2007. The main objectives of the study were to: - review the different factors affecting forest dieback in the EU and their related causes, - analyse and evaluate the effectiveness of available EU legislations and instruments to combat forest dieback in the EU and - examine the possibilities for establishing a specialised entity for forest protection. In the scope of the feasibility study a survey was conducted in the EU Member States on the importance of damaging agents in EU27 forests. The results of the survey show that the importance of individual threats to forest ecosystem health and vitality varies within European regions. Insects, storm/windfall, and fire were regarded as the most serious threats in Central Europe, Western Europe and Southern Europe respectively. Regional differences exist in relation to damage types and intensity, which thus reflect the importance for particular instruments to prevent, mitigate and control various causes of forest dieback. The feasibility study showed that at the EU level several efficient and well established measures have been implemented which contribute to the prevention, mitigation and control of forest dieback. The study showed also that as a consequence of the current state and the predicted development of environmental pressures, such as climate change, future activities on the EU level to combat forest dieback are urgently needed. Existing measures have to be further developed in order to (a) increase synergy effects between individual instruments, (b) make the instruments more transparent to the entire range of potential stakeholders and beneficiaries, and (c) improve the communication between the different actors involved. A major challenge will be to incorporate future patterns of forest dieback, into existing, amended or new measures. Only the triad of prevention, mitigation and control will put the EU into a position to maintain and enhance the multiple, beneficial functions of forests and their contribution to the quality of life.
South Tirol is an important region for apple production in Europe. The mild climate allows a high productivity but during the last decades, winter damage on apple trees was observed in 3 to 4 year intervals at numerous sites in South Tirol. This winter damage in apple orchards is economically relevant as e.g. in season 2004/2005 costs of more than 6 Mio Euros were caused. There are several indications that the observed dieback of crown parts or even trees was related to frost drought. The situation is comparable to that of trees at the timberline, where winter damage was analysed in previous projects. Based on our experience with trees growing at the alpine timberline, we hypothesize that winter damage in South Tirol apple orchards is strongly influenced by the duration of water uptake blockages, the extent of transpirational water losses, the trees water storage capacity as well as the climatic conditions in autumn. We expect damage in living tissues as well as xylem embolism to cause prolonged drought stress in spring. In the proposed project, these aspects will be analysed and avoidance strategies will be developed. In field measurements at five apple orchards in South Tirol, climatic conditions and effects on tree water relations (water potential, hydraulic conductivity, water storage, transpiration) as well as winter injury will be quantified, and in experimental approaches important parameters will be analysed in detail. These data will be compared with hydraulic characteristics (vulnerability to embolism, drought resistance of living tissues, water storage capacity) of studied varieties. In consequence, numerous varieties will be screened for resistance to frost drought, whereby hydraulic as well as related anatomical parameters will be analysed to develop a valuable screening protocol for variety selection. Cultivation techniques to avoid winter damage will also be tested in thi u.s.w.
At ANDRILL site SMS (Southern McMurdo Sound) an longer than 1000m sediment core will be drilled from a sea-ice platform covering Early/Middle Miocene (ca17 Ma) to Pleistocene strata of McMurdo Sound, Ross Sea, Antarctica. The target sediments were deposited on the western flank of the Victoria Land Basin (VLB), a structural half-graben that forms part of the West Antarctic Rift system, and experienced subsidence since late Eocene times. On this sediment core we propose to combine high-resolution on-ice measurement of chemical element concentrations using XRF core-scanner with off-ice high-precision chemical and sedimentological analysis on bulk samples (XRF, XRD, ICP-MS, biogenic components) and individual lithoclasts (LA-ICP-MS, electron microprobe, microscopy). The resulting multiple dataset will provide detailed information on sediment composition and, thus, contribute to several scientific objectives of ANDRILL such as the history of Ross/West Antarctic ice shelf expansion and retreat since ca17 million years, sea-ice presence/absence in the McMurdo region, and the history of Neogene sediment provenance and accumulation rates in the VLB. Our major goal is to improve our understanding of the Neogene paleoenvironmental evolution of Antarctica with a special focus on the Mid-Miocene climatic optimum (ca17-15 Ma) and the subsequent onset of major cooling (ca14 Ma) along with the key question on the stability of cold-polar climate conditions during the last 14 million years
Tephra layers in isce cores from Antarctica help to constrain corrleations between distant deep ice cores and represent important time markers in the case they can be related to an eruption of known age. These time markers can be combined with existing chemo-stratigraphic parameters such as stratigraphy based on ä18O and äD/H. To that end, we plan to determine major and trace element compositions, grain size and morphologxy of tephra layers from the deep ice cores EPICA-Dronning Maud Land and Dome Fuji (Dronning Maud Land). This data will be used for correlations to other ice cores from Marie Byrd Land (West Antarctica), Vostok and Dome C (Wilkes Land). Such data will also allow the identification of potential source areas for the tephra, e.g.volcanic regions in Antarctica (Ross Sea Rift, Marie Bird Land, South Shetland Islands) as well as New Zealand, Patagonia and the volcanic ozean islands in the southern oceans.
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