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  • 1
    Keywords: human ecology ; archaeology ; landscape assessment ; landscape changes ; humans ; nature ; Australia
    Description / Table of Contents: This impressive collection celebrates the work of Peter Kershaw, a key figure in the field of Australian palaeoenvironmental reconstruction. Over almost half a century his research helped reconceptualize ecology in Australia, creating a detailed understanding of environmental change in the Late Pleistocene and Holocene. Within a biogeographic framework one of his exceptional contributions was to explore the ways that Aboriginal people may have modified the landscape through the effects of anthropogenic burning. These ideas have had significant impacts on thinking within the fields of geomorphology, biogeography, archaeology, anthropology and history. Papers presented here continue to explore the dynamism of landscape change in Australia and the contribution of humans to those transformations. The volume is structured in two sections. The first examines evidence for human engagement with landscape, focusing on Australia and Papua New Guinea but also dealing with the human/environmental histories of Europe and Asia. The second section contains papers that examine palaeoecology and present some of the latest research into environmental change in Australia and New Zealand. Individually these papers, written by many of Australia’s prominent researchers in these fields, are significant contributions to our knowledge of Quaternary landscapes and human land use. But Peopled Landscapes also signifies the disciplinary entanglement that is archaeological and biogeographic research in this region, with archaeologists and environmental scientists contributing to both studies of human land use and palaeoecology. Peopled Landscapes reveals the interdisciplinary richness of Quaternary research in the Australasian region as well as the complexity and richness of the entangled environmental and human pasts of these lands.
    Pages: Online-Ressource (472 Seiten)
    ISBN: 9781921862724
    Language: English
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  • 2
    Keywords: Australia ; environment ; climate change ; biogeography ; palaeoecology ; human ecology
    Description / Table of Contents: Like a star chart this volume orientates the reader to the key issues and debates in Pacific and Australasian biogeography, palaeoecology and human ecology. A feature of this collection is the diversity of approaches ranging from interpretation of the biogeographic significance of plant and animal distributional patterns, pollen analysis from peats and lake sediments to discern Quaternary climate change, explanation of the patterns of faunal extinction events, the interplay of fire on landscape evolution, and models of the environmental consequences of human settlement patterns. The diversity of approaches, geographic scope and academic rigor are a fitting tribute to the enormous contributions of Geoff Hope. As made apparent in this volume, Hope pioneered multidisciplinary understanding of the history and impacts of human cultures in the Australia- Pacific region, arguably the globe’s premier model systems for understanding the consequences of human colonization on ecological systems. The distinguished scholars who have contributed to this volume also demonstrate Hope’s enduring contribution as an inspirational research leader, collaborator and mentor. Terra Australis leave no doubt that history matters, not only for land management, but more importantly, in alerting settler and indigenous societies alike to their past ecological impacts and future environmental trajectories.
    Pages: Online-Ressource (512 Seiten)
    ISBN: 9781921666810
    Language: English
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  • 3
    ISSN: 1442-9993
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Abstract  Fine-resolution palaeoecological and dendrochronological methods were used to investigate the impacts of climate change, and natural and anthropogenic disturbances on vegetation in the North Patagonian rainforest of southern Chile at decadal to century timescales during the late Holocene. A lake sediment mud–water interface core was collected from the northern Chonos Archipelago and analysed for pollen and charcoal. Dendrochronological analysis of tree cores collected from stands of Pilgerodendron uviferum close to the lake site was incorporated into the study. The combined analysis showed that the present mosaic of vegetation types in this region is a function of environmental changes across a range of timescales: millennial climate change, more recent natural and anthropogenic disturbances, and possibly short-term climatic variations. Of particular interest is the spatiotemporal distribution of Pilgerodendron uviferum dieback/burning in the Chonos Archipelago region.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Vegetation history and archaeobotany 4 (1995), S. 195-210 
    ISSN: 1617-6278
    Keywords: Pandanus ; Colocasia ; Pollen morphology ; New Guinea ; Early agriculture
    Source: Springer Online Journal Archives 1860-2000
    Topics: Archaeology , Biology
    Notes: Abstract Pollen records from the island of New Guinea, spanning the last 60 000 years, show a vegetation system sensitive to global climate change and strongly influenced by anthropogenic activity. The evidence for anthropogenic activity in pollen diagrams has focused on indirect indicators such as forest clearance, burning and increases in arable weeds. Tracing individual cultivars has proven to be very difficult as the major cultivated plants, in this case dominated by root crops, have low pollen production, are insect-pollinated or are harvested before flowering occurs. The identification of some cultivars is further restricted by limited information on pollen morphology. The pollen morphology of selected species from two genera (Pandanus and Colocasia), known to include important cultivated species, have been studied. Five pollen taxa are recognised after examination by light microscopy and scanning electron microscopy. It is shown that these can be easily distinguished on the broad criteria of pollen class, grain size and size of echini. The taxonomic and dispersal characteristics of the pollen morphology of these taxa are discussed and the implications of improved identification of cultivated species in late Quaternary pollen records are considered.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-06-27
    Description: A palynological record spanning the last glacial–interglacial period was derived from high-resolution, deep-sea core MD03-2607, located near Kangaroo Island in South Australia. The core site lies opposite the mouth of the River Murray that, together with the Darling River, drains the extensive (1.6 x 10⁶ km²) Murray Darling Basin (MDB). The record comprises 120 samples and is compared with detailed records of sea-surface temperature (SST), the C3/C4 plant ratio obtained from the δ¹³C of n-alkanes from leaf waxes, the fluvial clay fraction and its neodymium isotopic composition, airborne dust, as well as the biomass burning component levuglosan. The chronology of the core is robust; it is built on 24 radiocarbon dates derived from planktic foraminifera, 16 OSL dates, plus 12 tie points linked to the astronomically tuned marine isotopic record. Algal remains are found in nearly all samples supporting our postulation that the palynoflora is predominantly waterborne. Major findings are that the gymnosperm Callitris, together with high percentages of herb pollen (mostly C~3~ plants), is predominant during cold, arid phases, whereas Eucalyptus, is predominant during warmer and wetter periods. High charcoal concentration coincides with high percentages of Eucalyptus, mostly during wet and warm periods. Using the geochemistry of the core's fluvial sediments, it has been possible to identify when water-transported palynoflora and charcoal originated from the Murray sub-basin (consisting of the River Murray and its main tributaries but not from central or western South Australia). During those periods, rainfall principally originated from the southeastern Indian Ocean. When the Darling sub-basin was the main source of the palynoflora, rainfall must have instead originated from northern Australia. The eolian dust record from the core shows that the dust signal generally coincides with the increased values in herb pollen, in particular during the Last Glacial Maximum (LGM) when, in addition to high herb percentages, Callitris representation also increased. This dry landscape taxon likely colonised the then-exposed Lacepede Shelf during this period of extreme low sea level. There is a good correspondence between SST and mean annual precipitation reconstructed from the pollen counts. During warm phases in the ocean, Eucalyptus was the dominant tree taxon, especially for the entirety of MIS 5, plus MIS 3 and MIS 1. Charcoal levels were particularly low during the dry phases MIS 4 and 2, and even more so during the LGM.
    Keywords: Airborne dust; AUSCAN; C3/C4 plants; Callitris; CALYPSO; Calypso Corer; charcoal; Fluvial muds; Gyrostemon; Lacepede Shelf; Last glacial/interglacial cycle; levoglucosan; Marion Dufresne (1995); MD032607; MD03-2607; MD131; Murray Darling Basin; Neodymium isotopes; Southern Ocean; Ti/Ca
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
    Publication Date: 2023-06-27
    Keywords: AGE; Airborne dust; AUSCAN; C3/C4 plants; Callitris; CALYPSO; Calypso Corer; charcoal; DEPTH, sediment/rock; Fluvial muds; Gyrostemon; Lacepede Shelf; Last glacial/interglacial cycle; levoglucosan; Marion Dufresne (1995); MD032607; MD03-2607; MD131; Murray Darling Basin; Neodymium isotopes; Southern Ocean; Ti/Ca; Titanium/Aluminium ratio
    Type: Dataset
    Format: text/tab-separated-values, 3110 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Daniau, Anne-Laure; Bartlein, Patrick J; Harrison, S P; Prentice, Iain Colin; Brewer, Simon; Friedlingstein, Pierre; Harrison-Prentice, T I; Inoue, J; Izumi, K; Marlon, Jennifer R; Mooney, Scott D; Power, Mitchell J; Stevenson, J; Tinner, Willy; Andric, M; Atanassova, J; Behling, Hermann; Black, M; Blarquez, O; Brown, K J; Carcaillet, C; Colhoun, Eric A; Colombaroli, Daniele; Davis, Basil A S; D'Costa, D; Dodson, John; Dupont, Lydie M; Eshetu, Z; Gavin, D G; Genries, A; Haberle, Simon G; Hallett, D J; Hope, Geoffrey; Horn, S P; Kassa, T G; Katamura, F; Kennedy, L M; Kershaw, A Peter; Krivonogov, S; Long, C; Magri, Donatella; Marinova, E; McKenzie, G Merna; Moreno, P I; Moss, Patrick T; Neumann, F H; Norstrom, E; Paitre, C; Rius, D; Roberts, Neil; Robinson, G S; Sasaki, N; Scott, Louis; Takahara, H; Terwilliger, V; Thevenon, Florian; Turner, R; Valsecchi, V G; Vannière, Boris; Walsh, M; Williams, N; Zhang, Yancheng (2012): Predictability of biomass burning in response to climate changes. Global Biogeochemical Cycles, 26(4), https://doi.org/10.1029/2011GB004249
    Publication Date: 2024-01-13
    Description: We analyze sedimentary charcoal records to show that the changes in fire regime over the past 21,000 yrs are predictable from changes in regional climates. Analyses of paleo- fire data show that fire increases monotonically with changes in temperature and peaks at intermediate moisture levels, and that temperature is quantitatively the most important driver of changes in biomass burning over the past 21,000 yrs. Given that a similar relationship between climate drivers and fire emerges from analyses of the interannual variability in biomass burning shown by remote-sensing observations of month-by-month burnt area between 1996 and 2008, our results signal a serious cause for concern in the face of continuing global warming.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
    Publication Date: 2024-03-06
    Keywords: Acacia-type; AGE; Airborne dust; Algae; Alternanthera; Amaranthaceae/Chenopodiaceae; Amaryllidaceae/Liliaceae; Anthoceros-type; Apiaceae; Araucariaceae; Asteraceae Liguliflorae; Asteraceae Tubuliflorae; AUSCAN; Banksia; Botryococcus; C3/C4 plants; Callitris; Callitris-type; CALYPSO; Calypso Corer; Caryophyllaceae; Casuarina-type; Centrolepidaceae/Restionaceae; charcoal; Coelastrum; Convolvulaceae; Coprosma/Hedyotis-type; Cunoniaceae; Cyatheaceae; Cyperaceae; Dacrydium; Davallia-type; Debarya; DEPTH, sediment/rock; Dodonaea; Elaeocarpus; Epacris-type; Eucalyptus-type; Euphorbia-type; Ficus; Fluvial muds; Fungi spores; Geraniaceae; Gleicheniaceae; Gyrostemon; Haloragis; Herbs; Indeterminata; Lacepede Shelf; Lamiaceae; Last glacial/interglacial cycle; Leguminosae; Lemna; levoglucosan; Loranthaceae; Lycopodium (counted); Lycopodium spores per tablet; Lycopodium tablets; Malvaceae; Marion Dufresne (1995); MD032607; MD03-2607; MD131; Melaleuca/Myrtaceous, shrubs; Micrantheum-type; Monolete psilate; Moraceae/Urticaceae; Murray Darling Basin; Myoporaceae; Myriophyllum; Neodymium isotopes; Nothofagus; Phyllanthus; Phyllocladus; Plantago; Poaceae; Podocarpus; Podospora; Pollen, total; Polygala-type; Polypodiaceae; Potamogeton; Proteaceae; Pteridophyta; Pteridophyta indeterminata; Pteris; Ranunculaceae; Rhamnaceae; Rosaceae; Rumex; Rutaceae; Sample mass; Scaevola-type; Scrophulariaceae; Selaginella; Solanum-type; Sordaria; Southern Ocean; Spirogyra; Sporormiella; Theaceae; Thymelaeaceae; Ti/Ca; Trees and shrubs; Typha; Winteraceae; Zygnema
    Type: Dataset
    Format: text/tab-separated-values, 10406 data points
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  • 9
    Publication Date: 2024-03-06
    Keywords: Acacia-type; AGE; Airborne dust; Algae; Alternanthera; Amaranthaceae/Chenopodiaceae; Amaryllidaceae/Liliaceae; Anthoceros-type; Apiaceae; Araucariaceae; Asteraceae Liguliflorae; Asteraceae Tubuliflorae; AUSCAN; Banksia; Botryococcus; C3/C4 plants; Callitris; Callitris-type; CALYPSO; Calypso Corer; Caryophyllaceae; Casuarina-type; Centrolepidaceae/Restionaceae; charcoal; Charcoal; Coelastrum; Convolvulaceae; Coprosma/Hedyotis-type; Cunoniaceae; Cyatheaceae; Cyperaceae; Dacrydium; Davallia-type; Debarya; DEPTH, sediment/rock; Dodonaea; Elaeocarpus; Epacris-type; Eucalyptus-type; Euphorbia-type; Ficus; Fluvial muds; Fungi spores; Geraniaceae; Gleicheniaceae; Gyrostemon; Haloragis; Herbs; Indeterminable; Lacepede Shelf; Lamiaceae; Last glacial/interglacial cycle; Leguminosae; Lemna; levoglucosan; Loranthaceae; Lycopodium (counted); Lycopodium spores per tablet; Lycopodium tablets; Malvaceae; Marion Dufresne (1995); MD032607; MD03-2607; MD131; Melaleuca/Myrtaceous, shrubs; Micrantheum-type; Monolete psilate; Moraceae/Urticaceae; Murray Darling Basin; Myoporaceae; Myriophyllum; Neodymium isotopes; Nothofagus; Phyllanthus; Phyllocladus; Plantago; Poaceae; Podocarpus; Podospora; Pollen, total; Polygala-type; Polypodiaceae; Potamogeton; Proteaceae; Pteridophyta; Pteridophyta indeterminable; Pteris; Ranunculaceae; Rhamnaceae; Rosaceae; Rumex; Rutaceae; Sample mass; Scaevola-type; Scrophulariaceae; Selaginella; Solanum-type; Sordaria; Southern Ocean; Spirogyra; Sporormiella; Theaceae; Thymelaeaceae; Ti/Ca; Trees and shrubs; Typha; Winteraceae; Zygnema
    Type: Dataset
    Format: text/tab-separated-values, 10527 data points
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  • 10
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