澳大利亚东南部Werri Berri湖从土著到受欧洲影响的火灾制度的转变

IF 1.6 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL Holocene Pub Date : 2023-02-08 DOI:10.1177/09596836231151827
M. Constantine, Xiaohong Zhu, Haidee R. Cadd, S. Mooney
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引用次数: 3

摘要

在欧洲占领澳大利亚之前,火灾制度的驱动因素仍然存在争议,一些人主张由人为点火主导的制度,另一些人则主张气候来源或这些因素的混合。在这里,我们研究了澳大利亚东南部Werri Berri湖850年的消防制度历史,在欧洲占领之前和之后。宏观木炭和FTIR光谱用于推断湖泊附近的火灾状态的广泛变化。在850年的大部分时间里,我们发现几乎没有变化,最有趣的是,在土著居民最初的流离失所和欧洲人将农业和伐木引入该地区之后,没有明显的变化。从20世纪中期开始,燃烧面积和火灾严重程度或强度都有所增加,这可能是由于长时间降水增加和娱乐用地使用增加后燃料负荷和连通性增加的结果,这可能导致人为点火的增加。
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The transition from an Indigenous to a European influenced fire regime at Lake Werri Berri, south-east Australia
The drivers of fire regimes prior to the European occupation of Australia are still contentious, with some advocating regimes dominated by anthropogenic ignitions and others advocating a climate source or mixture of these elements. Here, we examine an 850-year history of fire regimes at Lake Werri Berri in south-east Australia, prior to and following European occupation. Macroscopic charcoal and FTIR spectroscopy were used to infer broad changes of the fire regime in proximity to the lake. We found little change through much of the 850-year period and most interesting, no apparent change following the initial displacement of Indigenous peoples and the introduction of farming and woodcutting to the region by Europeans. From the mid-20th Century onwards, there was an increase in both area burnt and fire severity or intensity, likely the result of increased fuel load and connectivity following an extended period of increased precipitation and heavier recreational land usage, which likely led to an increase in anthropogenic ignitions.
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来源期刊
Holocene
Holocene 地学-地球科学综合
CiteScore
4.70
自引率
8.30%
发文量
106
审稿时长
4 months
期刊介绍: The Holocene is a high impact, peer-reviewed journal dedicated to fundamental scientific research at the interface between the long Quaternary record and the natural and human-induced environmental processes operating at the Earth''s surface today. The Holocene emphasizes environmental change over the last ca 11 700 years.
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