Identifying the 'savanna' signature in lacustrine sediments in northern Australia
Bird, Michael I., Brand, Michael, Diefendorf, Aaron F., Haig, Jordahna L., Hutley, Lindsay B., Levchenko, Vladimir, Ridd, Peter V., Rowe, Cassandra, Whinney, James, Wurster, Christopher M., and Zwart, Costijn (2019) Identifying the 'savanna' signature in lacustrine sediments in northern Australia. Quaternary Science Reviews, 203. pp. 233-247.
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Abstract
This study reports palynological and geochemical results for modern and ancient sediments from 19 lakes on a rainfall gradient (784-1880 mm), across a range of savannas in Northern Australia. All proxies varied significantly across the range of sites examined, providing a robust envelope of values that can reliably be employed to identify a savanna signature in the sedimentary record. While the results indicate it is possible to identify a savanna, we found only three statistically significant relationships between any proxy measured in surface sediments and the major climate driver of savanna vegetation composition (rainfall amount). This is because edaphic factors play a dominant role in determining vegetation composition and also potentially because of the impact of land use change.
Measures of fire determined by charcoal counting were positively correlated with geochemical measures of pyrogenic carbon abundance, suggesting both record a similar signal. While measures of fire incidence were not correlated with rainfall, there was a significant positive correlation between charcoal abundance and number of fires early in the dry season, suggesting that charcoal abundance is controlled more by the number/timing of fires than climate. There was also a significant correlation between the delta C-13-value of pyrogenic carbon and tree:grass ratio derived from palynological indicators, indicating that the delta C-13-value of PyC is a reliable indicator of savanna 'woodiness'. Comparison of the carbon isotope composition of total organic carbon, PyC and n-alkanes between modern and Holocene sediments suggest that the savannas of the region have remained either similar in 'woodiness' or have thickened over the last millennia.
Item ID: | 56945 |
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Item Type: | Article (Research - C1) |
ISSN: | 1873-457X |
Keywords: | Quaternary, Paleoclimatology, Stable isotope, Palynology, Radiocarbon, Palaeoecology, Continental biomarkers, Southern Pacific, Vegetation dynamics |
Copyright Information: | (C) 2018 Elsevier Ltd. All rights reserved. |
Funders: | Innovative Research Universities of Australia Group, Australian Research Council (ARC), Centre for Accelerator Science |
Projects and Grants: | ARC DP130100334, ARC FL140100044 |
Date Deposited: | 23 Jan 2019 07:35 |
FoR Codes: | 37 EARTH SCIENCES > 3709 Physical geography and environmental geoscience > 370905 Quaternary environments @ 50% 37 EARTH SCIENCES > 3703 Geochemistry > 370303 Isotope geochemistry @ 50% |
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