Dan Penny

China and Southeast Asia

Publisher: Wiley

Date: 27-08-2012

DOI: 10.1002/9781118336311.CH6

Microfossil evidence of land-use intensification in north Thailand

Publisher: Elsevier BV

Date: 2005

DOI: 10.1016/J.JAS.2004.07.002

Clastic spring sediments: A tool for palaeoflood reconstruction?

Publisher: Schweizerbart

Date: 09-2012

DOI: 10.1127/0372-8854/2012/0081

A 3.5 ka record of paleoenvironments and human occupation at Angkor Borei, Mekong Delta, southern Cambodia

Publisher: Wiley

Date: 21-02-2003

DOI: 10.1002/GEA.10067

Reconstructing the history of environmental impact in a tropical mangrove ecosystem: A case study from the Suape port-industrial complex, Brazil

Publisher: Elsevier BV

Date: 05-2021

DOI: 10.1016/J.RSMA.2021.101747

Late Quaternary palaeoecology, palynology and palaeolimnology of a tropical lowland swamp: Rawa Danau, West-Java, Indonesia

Publisher: Elsevier BV

Date: 07-2001

DOI: 10.1016/S0031-0182(01)00245-0

Re-evaluating the occupation history of Koh Ker, Cambodia, during the Angkor period: A palaeo-ecological approach

Publisher: Public Library of Science (PLoS)

Date: 10-10-2018

DOI: 10.1371/JOURNAL.PONE.0203962

A 40,000 year palynological record from north-east Thailand; implications for biogeography and palaeo-environmental reconstruction

Publisher: Elsevier BV

Date: 07-2001

DOI: 10.1016/S0031-0182(01)00242-5

Luminescence dating of canal sediments from Angkor Borei, Mekong Delta, Southern Cambodia

Publisher: Elsevier BV

Date: 2007

DOI: 10.1016/J.QUAGEO.2006.05.032

Geoarchaeological evidence from Angkor, Cambodia, reveals a gradual decline rather than a catastrophic 15th-century collapse

Publisher: Proceedings of the National Academy of Sciences

Date: 25-02-2019

DOI: 10.1073/PNAS.1821460116

Abstract: Contrasting models exist to explain the movement of urban populations following the 15th-century demise of Angkor. Here we present geoarchaeological data from the urban core of Angkor that indicate a protracted decline in land use intensity during the 14th century rather than an abrupt demographic collapse. These results argue against traditional explanations for the demise of Angkor, which emphasize the role of interventionist foreign powers in forcing collapse, and imply a more complex and protracted transformation.

Pollen‐based reconstructions of biome distributions for Australia, Southeast Asia and the Pacific (SEAPAC region) at 0, 6000 and 18,000 ¹⁴C yr BP

Publisher: Wiley

Date: 24-08-2004

DOI: 10.1111/J.1365-2699.2004.01001.X

Iron and fire: Geoarchaeological history of a Khmer peripheral centre during the decline of the Angkorian Empire, Cambodia

Publisher: Elsevier BV

Date: 04-2016

DOI: 10.1016/J.JASREP.2016.01.028

Holocene palaeoenvironments and change at Three-Quarter Mile Lake, Silver Plains Station, Cape York Peninsula, Australia

Publisher: SAGE Publications

Date: 12-2006

DOI: 10.1177/0959683606069398

Abstract: Pollen and diatom analyses of organic sediments from Three-Quarter Mile Lake, a perched lake on Cape York Peninsula, north Queensland, indicate that significant changes in vegetation and hydrology occurred during the Holocene. Early Holocene grass-dominated landscapes were replaced in mid-Holocene times by increasingly woody vegetation comprising tropical heathlands, savanna and rainforest. Early-Holocene lake levels fluctuated widely. From mid-Holocene times, lake levels stabilized and water became increasingly acidic as a mature sw forest developed adjacent to the lake and contributed tannins to the lake water. The timing and character of changes are consistent with those described from the Atherton Tableland in wet tropical Queensland. Holocene dry phases described from the Northern Territory and the western shores of Cape York cannot be identified from Three-Quarter Mile Lake. Rainforest is currently close to its greatest Holocene extent, suggesting that the rainforest-dependent endemic fauna of northern Cape York have been isolated from rainforest blocks to the south throughout the last 10 000 years and, by inference, throughout at least the 120 000 years beyond that.

Long-term rates of sediment accumulation in the Tonle Sap, Cambodia: A threat to ecosystem health?

Publisher: Springer Science and Business Media LLC

Date: 2005

DOI: 10.1007/S10933-004-1323-2

The water management network of Angkor, Cambodia

Publisher: Cambridge University Press (CUP)

Date: 09-2008

DOI: 10.1017/S0003598X00097295

Abstract: Meticulous survey of the banks, channels and reservoirs at Angkor shows them to have been part of a large scale water management network instigated in the ninth century AD. Water collected from the hills was stored and could have been distributed for a wide variety of purposes including flood control, agriculture and ritual while a system of overflows and bypasses carried surplus water away to the lake, the Tonle Sap, to the south. The network had a history of numerous additions and modifications. Earlier channels both distributed and disposed of water. From the twelfth century onwards the large new channels primarily disposed of water to the lake. The authors here present and document the latest definitive map of the water network of Angkor.

Unearthing an Atlantean myth in Angkor: geoarchaeological investigation of the ‘underwater road’ crossing the Tonle Sap Lake, Cambodia

Publisher: Elsevier BV

Date: 08-2012

DOI: 10.1016/J.JAS.2012.04.005

Vegetation and land-use at Angkor, Cambodia: a dated pollen sequence from the Bakong temple moat

Publisher: Cambridge University Press (CUP)

Date: 09-2006

DOI: 10.1017/S0003598X00094060

Abstract: Investigating the use of land during the medieval period at the celebrated ceremonial area of Angkor, the authors took a soil column over 2.5m deep from the inner moat of the Bakong temple. The dated pollen sequence showed that the temple moat was dug in the eighth century AD and that the agriculture of the immediate area subsequently flourished. In the tenth century AD agriculture declined and the moat became choked with water-plants. It was at this time, according to historical documents, that a new centre at Phnom Bakeng was founded by Yasovarman I.

Metal enrichment in estuarine sediments proximal to acid sulfate soils as a novel palaeodrought proxy

Publisher: Elsevier BV

Date: 2018

DOI: 10.1016/J.SCITOTENV.2017.08.157

Abstract: Persistent drought over eastern Australia at the turn of the last millennium reduced stream flow in Australia's largest and most economically important drainage basin. Low water levels in the basin's terminal lakes triggered widespread pyrite oxidation, which altered surface water chemistry and released metals into the environment. The frequency of these events, and the links between drought and acid sulfate soil activation, are not known because the historical and instrumental records are short. Here, we present a Holocene-aged record of trace metal enrichment from Lake Albert-part of the terminal Lower Lakes system of the Murray-Darling Basin, Australia-that demonstrates the potential of trace elements mobilised during acidification events for palaeodrought reconstructions. Symptomatic metals were measured from a core of clayey sediment to form a multi-element assemblage that reveals acidification events in the geological past. Correlation with regional climate proxies suggests that climate forcing is significant in driving metal flux to estuarine sinks in acid sulfate soil rich landscapes, although the intensity of a drought is not the only variable responsible for acidification intensity. The constructed record indicates that regional climate moved from a generally humid climate phase with intermittent droughts, to a more arid climate at ~5.2ka which prevailed until ~1.7ka. Following conditions were relatively wet with low climatic variability through till European Settlement. Enrichment is observed coincident with both the 1982-83 drought and Millennium Drought, the latter of which reaching an intensity unsurpassed in the last ~4.8ka, likely a product of anthropogenic changes to the Lower Murray-Darling Basin system.

Historical socioecological transformations in the global tropics as an Anthropocene analogue

Publisher: Proceedings of the National Academy of Sciences

Date: 27-09-2021

DOI: 10.1073/PNAS.2022211118

Abstract: Large, low-density settlements of the tropical world disintegrated during the first and second millennia of the CE. This phenomenon, which occurred in South Asia, Southeast Asia, and Mesoamerica, is strongly associated with climate variability and extensive landscape transformation. These profound social transformations in the tropical world have been popularized as “collapse,” yet archaeological evidence suggests a more complex and nuanced story characterized by persistence, adaptation, and resilience at the local and regional scales. The resulting tension between ideas of climate-driven collapse and evidence for erse social responses challenges our understanding of long-term resilience and vulnerability to environmental change in the global tropics. Here, we compare the archetypal urban collapse of the Maya, in modern Belize, Guatemala, Honduras, and Mexico, during the 8th to 11th centuries CE, and the Khmer in modern Cambodia, Laos, Thailand, and Vietnam during the 14th to 15th centuries CE. We argue that the social response to environmental stress is spatially and temporally heterogenous, reflecting the generation of large-scale landesque capital surrounding the urban cores. Divergences between vulnerable urban elite and apparently resilient dispersed agricultural settlements sit uncomfortably with simplistic notions of social collapse and raise important questions for humanity as we move deeper into the Anthropocene.

The use of AMS ¹⁴C dating to explore issues of occupation and demise at the medieval city of Angkor, Cambodia

Publisher: Elsevier BV

Date: 06-2007

DOI: 10.1016/J.NIMB.2007.02.095

Distinguishing the pollen of Dipterocarpaceae from the seasonally dry and moist tropics of south-east Asia using light microscopy

Publisher: Elsevier BV

Date: 04-2019

DOI: 10.1016/J.REVPALBO.2019.01.012

The environmental context of a city in decline: The vegetation history of a Khmer peripheral settlement during the Angkor period

Publisher: Elsevier BV

Date: 04-2019

DOI: 10.1016/J.JASREP.2019.01.006

The Mekong at climatic crossroads: Lessons from the geological past

Publisher: Royal Swedish Academy of Sciences

Date: 05-2008

DOI: 10.1579/0044-7447(2008)37[164:TMACCL]2.0.CO;2

Abstract: The wetlands of the lower Mekong River Basin are ecologically and socioeconomically significant, but they are threatened by predicted climatic change. The likely response of wetland ecosystems to altered flooding regimes and surface-water chemistry is unknown in detail and difficult to model. One way of exploring the impact of climate change on wetland ecosystems is to utilize proxy environmental data that reveal patterns of change over geological time. In recent years, the coverage and resolution of proxy climatic data have improved markedly in the region. Recent evidence of the South China Sea transgression into southern and central Cambodia and paleobotanical evidence from the Tonle Sap ("Great Lake") and elsewhere allow us to explore how periods of higher-than-present sea level and increased monsoon rainfall in the past have impacted the wetland ecology of the lower Mekong River Basin.

Ecological history of Lachlan Nature Reserve, Centennial Park, Sydney, Australia: a palaeoecological approach to conservation

Publisher: Cambridge University Press (CUP)

Date: 08-04-2014

DOI: 10.1017/S0376892914000083

Abstract: Reconstructing the environmental history of protected areas permits an empirically-based assessment of the conservation values ascribed to these sites. Ideally, this long-term view can contribute to evidence-based management policy that is both ecologically ‘realistic’ and pragmatically feasible. Lachlan Nature Reserve, a protected wetland in Centennial Park, Sydney, is claimed to be the final remnant of early and pre-European sw lands that were once extensive in the area, and the site is thus considered to have indigenous cultural and natural conservation significance. This study uses palynological techniques to reconstruct vegetation communities at the Reserve from the late Holocene to the present in order to assess whether these values adequately reflect the history, character and development of the site. The findings indicate that the modern site flora is a modified Melaleuca quinquenervia low forest assemblage formed in response to aggregated anthropogenic disturbance since colonial settlement. This assemblage replaces an Epacris -dominated heath-sw land community that was extirpated in the mid-20th century. These results emphasize the value of long-term studies in contributing to a realistic management policy that explicitly reflects the normative basis of conservation, and values the influence of past land-uses on contemporary protected ecosystems.

Geochemical signatures of acidic drainage recorded in estuarine sediments after an extreme drought

Publisher: Elsevier BV

Date: 12-2020

DOI: 10.1016/J.SCITOTENV.2020.141435

Forest, fire & monsoon: investigating the long-term threshold dynamics of south-east Asia’s seasonally dry tropical forests

Publisher: Elsevier BV

Date: 06-2020

DOI: 10.1016/J.QUASCIREV.2020.106334

Forests, Palms, and Paddy Fields

Publisher: Routledge

Date: 05-04-2023

DOI: 10.4324/9781351128940-11

Climate as a contributing factor in the demise of Angkor, Cambodia

Publisher: Proceedings of the National Academy of Sciences

Date: 29-03-2010

DOI: 10.1073/PNAS.0910827107

Abstract: The “hydraulic city” of Angkor, the capitol of the Khmer Empire in Cambodia, experienced decades-long drought interspersed with intense monsoons in the fourteenth and fifteenth centuries that, in combination with other factors, contributed to its eventual demise. The climatic evidence comes from a seven-and-a-half century robust hydroclimate reconstruction from tropical southern Vietnamese tree rings. The Angkor droughts were of a duration and severity that would have impacted the sprawling city’s water supply and agricultural productivity, while high-magnitude monsoon years damaged its water control infrastructure. Hydroclimate variability for this region is strongly and inversely correlated with tropical Pacific sea surface temperature, indicating that a warm Pacific and El Niño events induce drought at interannual and interdecadal time scales, and that low-frequency variations of tropical Pacific climate can exert significant influence over Southeast Asian climate and society.

An integrated palaeoenvironmental record of Early Modern occupancy and land use within Angkor Thom, Angkor

Publisher: Elsevier BV

Date: 2021

DOI: 10.1016/J.QUASCIREV.2020.106710

The demise of Angkor: Systemic vulnerability of urban infrastructure to climatic variations

Publisher: American Association for the Advancement of Science (AAAS)

Date: 05-10-2018

DOI: 10.1126/SCIADV.AAU4029

Abstract: The historic urban collapse of Angkor is linked to infrastructural complexity and climatic variability.

'Here be dragons': Integrating scientific data and place-based observation for environmental management

Publisher: Elsevier BV

Date: 08-2016

DOI: 10.1016/J.APGEOG.2016.06.002

Persistence of wetlands on North Stradbroke Island (south-east Queensland, Australia) during the last glacial cycle: implications for Quaternary science and biogeography

Publisher: Wiley

Date: 08-2017

DOI: 10.1002/JQS.2981

Terrestrial biosphere changes over the last 120 kyr

Publisher: Copernicus GmbH

Date: 18-01-2016

DOI: 10.5194/CP-12-51-2016

Abstract: Abstract. A new global synthesis and biomization of long ( 40 kyr) pollen-data records is presented and used with simulations from the HadCM3 and FAMOUS climate models and the BIOME4 vegetation model to analyse the dynamics of the global terrestrial biosphere and carbon storage over the last glacial–interglacial cycle. Simulated biome distributions using BIOME4 driven by HadCM3 and FAMOUS at the global scale over time generally agree well with those inferred from pollen data. Global average areas of grassland and dry shrubland, desert, and tundra biomes show large-scale increases during the Last Glacial Maximum, between ca. 64 and 74 ka BP and cool substages of Marine Isotope Stage 5, at the expense of the tropical forest, warm-temperate forest, and temperate forest biomes. These changes are reflected in BIOME4 simulations of global net primary productivity, showing good agreement between the two models. Such changes are likely to affect terrestrial carbon storage, which in turn influences the stable carbon isotopic composition of seawater as terrestrial carbon is depleted in 13C.

A 4700-year record of hydroclimate variability over the Asian monsoon intersection zone inferred from multi-proxy analysis of lake sediments

Publisher: Elsevier BV

Date: 03-2019

DOI: 10.1016/J.GLOPLACHA.2018.12.009

A combined pollen and phytolith record for fourteen thousand years of vegetation change in northeastern Thailand

Publisher: Elsevier BV

Date: 09-1998

DOI: 10.1016/S0034-6667(98)00029-3

Assessment of the temporal retention of mercury and nutrient records within the mangrove sediments of a highly impacted estuary

Publisher: Elsevier BV

Date: 04-2022

DOI: 10.1016/J.ENVRES.2021.112569

Abstract: Mangrove ecosystems are dynamic and bio erse environments with the capacity to sequester more organic carbon per unit area, per time, than terrestrial forests, yet are among one of the most heavily degraded ecosystems on Earth. Here, we quantify trace metal, nutrient and carbon accumulation rates in a tropical mangrove environment in northeast Brazil, a region that has been rapidly developed over the past seven decades. Carbon accumulation rate results show modest or no increase since the 1950's, when major development occurred in the region. Organic carbon isotope (δ

The environmental impact of Cambodia's ancient city of Mahendraparvata (Phnom Kulen)

Publisher: Public Library of Science (PLoS)

Date: 08-01-2014

DOI: 10.1371/JOURNAL.PONE.0084252

The Holocene history and development of the Tonle Sap, Cambodia

Publisher: Elsevier BV

Date: 02-2006

DOI: 10.1016/J.QUASCIREV.2005.03.012

An Environmental History of Angkor

Publisher: Routledge

Date: 05-04-2023

DOI: 10.4324/9781351128940-3

Multi-stage Holocene evolution of the River Murray Estuary, South Australia

Publisher: SAGE Publications

Date: 08-10-2020

DOI: 10.1177/0959683620961487

Abstract: The River Murray Estuary, South Australia exhibits a morphology typical of a wave-dominated estuary and comprises two large, shallow central basin lakes – Lakes Alexandrina and Albert. Contested interpretations of the estuary’s limnological history and uncertainty surrounding the sustainability of current basin water usage practice warrant a robust investigation into how the system has evolved. Here we combine lithostratigraphic, geochemical and sedimentological evidence from a transect of sediment cores to reconstruct the sediment infill history of the system. We uncover multiple stages of sediment infill over the history of the system, associated with (1) the low gradient morphology of the estuary and lower river channel, (2) the mid- to late-Holocene sea-level regression and (3) anthropogenic modifications to the fluvio-estuarine system. We show that while estuarine conditions in the system were fully established during the mid-Holocene highstand (~6.4 kyr BP), central basin facies sedimentation was focussed further inland before prograding with the lowering of base level and shifting of tidal influence as sea-level fell. Central basin facies sedimentation within northern Lake Albert occurred from 5.4 to 4.0 cal kyr BP at ~0.25 cm yr -1 . The uppermost accumulation of this unit was eroded by continued reduction in base level until sea-level regression concluded at 3.5 cal kyr BP. Barrage and weir installation (1940 CE) re-initiated and expanded central basin facies sedimentation in the estuary (~0.32 cm yr -1 ). Recently deposited sediments exhibit geochemical markers of increased trophy and more frequent acid sulfate soil acidification, exposing human impacts on the estuary.

The use of diatoms to assess past and present water quality

Publisher: Wiley

Date: 03-1995

DOI: 10.1111/J.1442-9993.1995.TB00522.X

Claiming the hydraulic network of Angkor with Viṣṇu: A multidisciplinary approach including the analysis of archaeological remains, digital modelling and radiocarbon dating: With evidence for a 12th century renovation of the West Mebon

Publisher: Elsevier BV

Date: 10-2016

DOI: 10.1016/J.JASREP.2016.06.031

The effect of proximity to protected areas on community adaptation to environmental change

Publisher: Elsevier BV

Date: 2022

DOI: 10.1016/J.JENVMAN.2021.113805

Abstract: The consequences of protected areas for proximal human communities are erse. Protected areas can alleviate poverty by providing a range of economic opportunities for people that live and work within them. Equally, however, they may also disempower and disposes local communities. For communities adapting to systemic environmental change, proximity to protected areas can act to limit potential adaptive pathways. Here, we employ social science methods to explore the impact of an internationally significant protected area on adjacent communities in the Tonle Sap Lake basin, Cambodia. Semi-structured interviews, informed by a scenario framework, reveal an awareness of declining fish yields and a perceived lack of economic alternatives. Vulnerability to hydroclimatic extremes, particularly storms, flood, drought and - increasingly - fire, are exacerbated as a result of proximity to the protected area. We conclude that the impact of protected areas on local communities is heterogenous, and that the development of adaptive and effective management policies requires sensitivity to local conditions and impacts.

Radiocarbon Dating of a Speleothem Record of Paleoclimate for Angkor, Cambodia

Publisher: Cambridge University Press (CUP)

Date: 12-2017

DOI: 10.1017/RDC.2017.115

Abstract: We report the chronological construction for the top portion of a speleothem, PC1, from southern Cambodia with the aim of reconstructing a continuous high-resolution climate record covering the fluorescence and decline of the medieval Khmer kingdom and its capital at Angkor (~9th–15th centuries AD). Earlier attempts to date PC1 by the standard U-Th method proved unsuccessful. We have therefore dated this speleothem using radiocarbon. Fifty carbonate s les along the growth axis of PC1 were collected for accelerator mass spectrometry (AMS) analysis. Chronological reconstruction for PC1 was achieved using two different approaches described by Hua et al. (2012a) and Lechleitner et al. (2016a). Excellent concordance between the two age-depth models indicates that the top ~47 mm of PC1 grew during the last millennium with a growth hiatus during ~1250–1650 AD, resulting from a large change in measured 14 C values at 34.4–35.2 mm depth. The timing of the growth hiatus covers the period of decades-long droughts during the 14th–16th centuries AD indicated in regional climate records.

Vegetation changes from the late Pleistocene through the Holocene from three areas of archaeological significance in Thailand

Publisher: Elsevier BV

Date: 2004

DOI: 10.1016/J.QUAINT.2003.09.001

Sediment: Curse or Blessing for Tonle Sap Lake?

Publisher: Royal Swedish Academy of Sciences

Date: 05-2008

DOI: 10.1579/0044-7447(2008)37[158:SCOBFT]2.0.CO;2

Abstract: It has been claimed that Tonle Sap Lake is rapidly filling with sediment as a result of increasing sediment yields from the catchment. Infilling of the lake basin would have serious implications for the magnitude of flooding in central Cambodia and the Mekong Delta region and threaten the lake's unique ecosystem. In this article, we synthesize the results of radiocarbon dating of sediment cores and hydrodynamic modeling results to provide an empirically based assessment of this issue. We find that current sedimentation rates within the lake basin proper are low and have been for several millennia. However, sedimentation at the lake margin and in its floodplain is relatively high, which presents a range of issues for riparian communities.

University Of Sydney

Location: Australia

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Monash University

Location: Australia

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The University Of Edinburgh

Location: United Kingdom of Great Britain and Northern Ireland

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Resolving The Maya Climate-collapse Hypothesis

Start Date: 2018

End Date: 2020

Funder: Australian Research Council

The Historical Environment Of Angkor: An Investigation Of Synergy Between People And Landscape

Start Date: 2002

End Date: 2002

Funder: Australian Research Council

Urban Infrastructure, Inertia And Ecology: The Growth And Decline Of Angkor, Cambodia (9th To 16th Century AD)

Start Date: 2005

End Date: 2009

Funder: Australian Research Council

The Late Pleistocene Peopling Of East Asia And Associated Climate-Environment History

Start Date: 2008

End Date: 2012

Funder: Australian Research Council

Thresholds And Hysteresis: How Do Abrupt Changes In The Asian Monsoon Affect Ecosystems And Environmental Processes?

Start Date: 2010

End Date: 2012

Funder: Australian Research Council

Integrated Vibrational Spectroscopic Mapping For Archeological, Biological, Geological, Materials, And Medical Research

Start Date: 2008

End Date: 2008

Funder: Australian Research Council

Urbanism After Angkor (14th-18th Century)

Start Date: 2017

End Date: 2021

Funder: Australian Research Council

(High-resolution ITRAX XRF Core Scanning Facility For Global Change Research)

Start Date: 2010

End Date: 2010

Funder: Australian Research Council

Discovery Projects - Grant ID: DP1094367

Start Date: 02-2010

End Date: 2015

Amount: $285,000.00

Funder: Australian Research Council

Discovery Projects - Grant ID: DP0211600

Start Date: 07-2002

End Date: 06-2003

Amount: $45,000.00

Funder: Australian Research Council

Discovery Projects - Grant ID: DP0558130

Start Date: 2005

End Date: 12-2009

Amount: $1,002,630.00

Funder: Australian Research Council

Discovery Projects - Grant ID: DP180101986

Start Date: 2018

End Date: 12-2023

Amount: $208,846.00

Funder: Australian Research Council

Discovery Projects - Grant ID: DP0877603

Start Date: 09-2008

End Date: 12-2012

Amount: $665,000.00

Funder: Australian Research Council

Linkage Infrastructure, Equipment And Facilities - Grant ID: LE100100141

Start Date: 2010

End Date: 12-2010

Amount: $420,000.00

Funder: Australian Research Council

Linkage Infrastructure, Equipment And Facilities - Grant ID: LE0883036

Start Date: 01-2008

End Date: 10-2008

Amount: $400,000.00

Funder: Australian Research Council

Discovery Projects - Grant ID: DP170102574

Start Date: 2017

End Date: 06-2024

Amount: $787,945.00

Funder: Australian Research Council