Resource Management and Geography - Research Publications

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    Hope, despair and transformation: Climate change and the promotion of mental health and wellbeing.
    Fritze, JG ; Blashki, GA ; Burke, S ; Wiseman, J (Springer Science and Business Media LLC, 2008-09-17)
    BACKGROUND: This article aims to provide an introduction to emerging evidence and debate about the relationship between climate change and mental health. DISCUSSION AND CONCLUSION: The authors argue that:i) the direct impacts of climate change such as extreme weather events will have significant mental health implications;ii) climate change is already impacting on the social, economic and environmental determinants of mental health with the most severe consequences being felt by disadvantaged communities and populations; iii) understanding the full extent of the long term social and environmental challenges posed by climate change has the potential to create emotional distress and anxiety; and iv) understanding the psycho-social implications of climate change is also an important starting point for informed action to prevent dangerous climate change at individual, community and societal levels.
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    The Revenge of the Still
    BISSELL, D ; FULLER, G (M/C - Media and Culture, 2009)
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    A 5600-yr history of changing vegetation, sea levels and human impacts from the Black Sea coast of Georgia
    Connor, SE ; Thomas, I ; Kvavadze, EV (SAGE PUBLICATIONS LTD, 2007)
    Mid-late Holocene pollen evidence from the Ispani-II Sphagnum bog in lowland Western Georgia shows that 4500 years ago Castanea (chestnut)-dominated woods rapidly declined to be replaced by alder swamps and, later, during the first millennium be, by open, marshy landscapes in which fire played a prominent part. Around 1900 years ago, Sphagnum blanket bog encroached on the marshes and dense Fagus-Carpinus (beech-hornbeam) forest enveloped the surrounding land. This vegetation remained until the mid-twentieth century, when forests were clear-felled and marshes were drained for large-scale, mechanized agriculture. Previous studies have emphasized climate's governing role in setting the course of Holocene vegetation development in lowland Western Georgia, but our results provide little support for this hypothesis. To a much greater degree, episodes of coastal subsidence, sea-level rise and human impact have shaped the vegetation history of coastal Western Caucasus.
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    Calluna vulgaris and Spiranthes amoena in the Colchis mire flora: weeds or relicts?
    Arabuli, GIORGIJ ; Connor, SIMONE ; Kvavadze, ELISOV (Sciendo (De Gruyter), 2007)
    ecent botanical discoveries in the Colchis lowland of Western Georgia have renewed interest in the extensive Sphagnum peat bogs along the Black Sea coast. This area has long been recognized as an important refugium for thermophilous, Tertiary relict plants, but is also home to some plants typical of the boreal zone. In this paper, we present palynological and historical data that calls into question the idea that Calluna vulgaris (L.) Hull and Spiranthes amoena (Bieb.) Spreng., the Euro-Siberian elements recently discovered in the Colchis Sphagnum bogs, are adventive. We argue instead that they are relicts of late Pleistocene age that elsewhere in the Western Asia were pushed out by afforestation and sea-level rise during the early-mid Holocene.
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    A survey of modern pollen and vegetation along an altitudinal transect in southern Georgia, Caucasus region
    Connor, SE ; Thomas, I ; Kvavadze, EV ; Arabuli, GJ ; Avakov, GS ; Sagona, A (ELSEVIER SCIENCE BV, 2004)
    This paper describes the pollen representation of vegetation patterns along an altitudinal transect in the South Caucasus region. Surface sediments from eight small- to medium-sized lakes and wetlands were analysed for modern pollen, and the results analysed numerically using detrended correspondence analysis (DCA) and dichotomised ordination (TWINSPAN). Pollen spectra from the semidesert region have a clear palynological signal characterised by an abundance of Chenopodiaceae. Differentiation of oak forest, upper tree-line and subalpine communities is more difficult: all are dominated by arboreal pollen (AP) types. The authors propose a number of indicator pollen types and pollen threshold values that may assist in detecting tree-line variations and deforestation events in Holocene pollen diagrams.
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    Climatic and human influences on vegetation dynamics around Tbilisi over the past 6000 years
    Connor, SE ; Kvavadze, EV (Georgian Academy of Sciences, 2005)
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    Sediments as archives of industrialisation: evidence of atmospheric pollution in coastal wetlands of southern Sydney, Australia
    CONNOR, S ; Thomas, I (Springer, 2003)
    The history of heavy metal pollution in southern Sydney was reconstructed from wetland sediments using chemical analysis. Seven wetlands along the Pacific coast were examined for present day concentrations of acid-extractable Cd, Cu, Fe, Pb and Zn. Additionally, four of these sites were cored in order to assess past levels of these metal contaminants, changes in organic content and magnetic susceptibility variations. The low nutrient status and closed catchments of the study sites suggested that the pollutants were predominantly derived from atmospheric sources. Surficial sediments were enriched with Cd, Cu, Fe, Pb and Zn levels 5.0, 16.4, 22.7, 8.2 and 22.5 times baseline levels, respectively. In some cases, the concentrations of trace metals were in excess of environmentally acceptable levels. The results show a strong spatial association between sources and levels of pollutants, and the increase in metals levels in sedimentary records corresponds well to documentary historical evidence.This study demonstrates the utility of coastal wetlands in the reconstruction of atmospheric pollution histories, and their particular vulnerability to contamination from airborne pollutants in urban areas.
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    Modelling late Quaternary changes in plant distribution, vegetation and climate using pollen data from Georgia, Caucasus
    Connor, SE ; Kvavadze, EV (WILEY, 2009-03)
    To use pollen data, numerical analysis and modelling to reconstruct late Quaternary vegetation and climate in a complex, mountainous environment. Georgia (Caucasus region). Pollen data were assembled from various sources and used to map: (1) changing frequencies of individual taxa; (2) vegetation changes; and (3) reconstructed climatic parameters for the past 14,000 years. Numerical analyses were performed using two-way indicator species analysis ( twinspan), detrended correspondence analysis (DCA), the modern analogue technique (MAT) and weighted averaging (WA). Mapping of pollen taxa showed that Chenopodiaceae, Artemisia and Ephedra were most abundant in the study area during the late-glacial. Betula and Corylus expanded during the early Holocene, yielding to Abies, Carpinus, Fagus, Quercus and Castanea. Picea, Pinus, Juglans and Ostrya-type expanded during the late Holocene. Mixed forests grew in the moist, Black Sea refugium throughout the late Quaternary. Elsewhere in Georgia, the Pleistocene-Holocene transition is recorded as a shift from desert-steppes to oak-xerophyte communities and mixed forests. This kind of vegetation remained relatively stable until the mid-late Holocene, when coniferous forests and mountain grasslands advanced. DCA showed that rainfall was most strongly correlated with pollen composition in the study area (r² = 0.55). No temperature signal was detected. A weighted-averaging transfer function linking pollen percentages to annual precipitation was selected over a MAT model as it performed better when applied to a validation data set. Rainfall reconstructions indicate widespread aridity at the terminal Pleistocene, followed by a gradual increase in precipitation, peaking during the mid Holocene (7000-4000 cal. yr bp) and generally decreasing thereafter. On a regional scale, the results confirm those from previous studies of palaeovegetation and palaeoclimate in Western Asia. On a local scale, reconstructions from individual sites often diverge from the regional trend because of edaphic changes, ecological succession, human impacts and other disturbances. Some of these factors are probably responsible for the increasing heterogeneity of Georgia's vegetation in the latter half of the Holocene.
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