Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/12025
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dc.contributor.authorSamuel, KM-
dc.contributor.authorReynolds, W-
dc.contributor.authorMay, JH-
dc.contributor.authorForbes, MS-
dc.contributor.authorStromsoe, N-
dc.contributor.authorFletcher, MS-
dc.contributor.authorCohen, T-
dc.contributor.authorMoss, PT-
dc.contributor.authorMazumder, D-
dc.contributor.authorGadd, PS-
dc.date.accessioned2021-10-21T00:45:11Z-
dc.date.available2021-10-21T00:45:11Z-
dc.date.issued2021-12-01-
dc.identifier.citationSamuel, K. M., Reynolds, W., May, J.-H., Forbes, M. S., Stromsoe, N., Fletcher, M.-S., Cohen, T., Moss, P., Mazumder, D. & Gadd, P. (2021).Ecosystem and landscape change in the ‘Top End’ of Australia during the past 35 kyr, Palaeogeography, Palaeoclimatology, Palaeoecology, 583,110659. doi:10.1016/j.palaeo.2021.110659en_US
dc.identifier.issn0031-0182-
dc.identifier.urihttps://doi.org/10.1016/j.palaeo.2021.110659en_US
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/12025-
dc.descriptionThe attached PDF is the post print version of this article.en_US
dc.description.abstractThe Indo-Australian Summer Monsoon (IASM) is the dominant climate feature of northern Australia, affecting rainfall/runoff patterns over a large portion of the continent and exerting a major control on the ecosystems of the Australia's Top End, including the viability of wetland ecosystems and the structure of the woody savanna, which characterises Northern Australia. We examined the behaviour the IASM from 35 ka using proxy data preserved in the sediments of Table Top Swamp, a small seasonal swamp in northern Australia. Elemental data, stable C and N isotopes, pollen and sedimentary data were combined to develop a picture of monsoon activity and ecosystem response. Results demonstrated that between 35 and 25 ka conditions were drier and more stable than present, with a more grass dominated savanna and limited wetland development, implying reduced IASM activity. After ~25 ka, there is evidence of increased moisture at the study site, but also increased IASM variability. However, despite evidence of at least periodic increases in moisture, including periods of wetland establishment, the IASM displayed a subdued response to peak precession insolation forcing by comparison to the other global monsoon systems. Instead, the greatest change occurred from ~10 ka when the continental shelf flooded, increasing moisture advection to the study site and resulting in establishment of a quasi-permeant wetland. Whereas the early Holocene was marked by both the onset of pollen preservation and a wetter vegetation mosaic, indicative of a consistently active IASM, the mid-late Holocene was marked by drier vegetation, increased fire, but also increased C3 vegetation and runoff, implying increased IASM variability. Holocene changes in ecosystem dynamics occur coincident with an expansion in human population, which likely also influenced vegetation and landscape response at the study site. © 2021 Elsevier B.V.en_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectStable isotopesen_US
dc.subjectPollenen_US
dc.subjectWetlandsen_US
dc.subjectFiresen_US
dc.subjectEcosystemsen_US
dc.subjectSea levelen_US
dc.subjectAustraliaen_US
dc.titleEcosystem and landscape change in the ‘Top End’ of Australia during the past 35 kyren_US
dc.typeJournal Articleen_US
dc.date.statistics2021-09-28-
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