Fire, humans and climate as drivers of environmental change on Broughton Island, New South Wales, Australia
dc.contributor.author | Mooney, Scott | |
dc.contributor.author | Hope, Geoffrey | |
dc.contributor.author | Horne, Dylan | |
dc.contributor.author | Kamminga, Johan | |
dc.contributor.author | Williams, Alan N. | |
dc.date.accessioned | 2022-04-27T05:20:13Z | |
dc.date.issued | 2020 | |
dc.date.updated | 2020-12-27T07:20:43Z | |
dc.description.abstract | In Australia, the drivers of precolonial fire regimes remain contentious, with some advocating an anthropogenic-dominated regime, and others highlighting the importance of climate, climatic variability or alternatively some nexus between climate and human activity. Here, we explore the inter-relationships between fire, humans and vegetation using macroscopic charcoal, archaeology and palynology over the last ~5430 cal. year BP from Broughton Island, a small, near-shore island located in eastern Australia. We find a clear link between fire and the reduction of arboreal pollen and rainforest indicators on the island, especially at ~4.0 ka and in the last ~1000years. Similarities with comparable palaeoenvironmental records of fire in the region and a record of strong El Nino (dry, fire-prone) events supports the contention that climate was a significant influence on the fire regimes of Broughton Island. However, two periods of enhanced fire activity, at ~4000 years BP and ~<600 years BP have weaker links to climate, and perhaps reflect anthropogenic activity. Changes to the fire regime in the last ~600years corresponds with the earliest evidence of Indigenous archaeology on the island, and coincides with implications that Polynesian people were present in the region. After the mid-Twentieth Century a human-dominated fire regime is also an obvious feature of the reconstructed fire record on Broughton Island. | en_AU |
dc.format.mimetype | application/pdf | en_AU |
dc.identifier.issn | 1477-0911 | en_AU |
dc.identifier.uri | http://hdl.handle.net/1885/264127 | |
dc.language.iso | en_AU | en_AU |
dc.publisher | Sage Publications Inc | en_AU |
dc.rights | © 2020 The authors | en_AU |
dc.source | The Holocene | en_AU |
dc.subject | charcoal | en_AU |
dc.subject | palynology | en_AU |
dc.subject | eastern Australia | en_AU |
dc.subject | ENSO | en_AU |
dc.subject | Aboriginal | en_AU |
dc.subject | mid-to-late-Holocene | en_AU |
dc.title | Fire, humans and climate as drivers of environmental change on Broughton Island, New South Wales, Australia | en_AU |
dc.type | Journal article | en_AU |
dcterms.accessRights | Open Access via publisher website | en_AU |
local.bibliographicCitation.issue | 11 | en_AU |
local.bibliographicCitation.lastpage | 1539 | en_AU |
local.bibliographicCitation.startpage | 1528 | en_AU |
local.contributor.affiliation | Mooney, Scott, University of New South Wales | en_AU |
local.contributor.affiliation | Hope, Geoffrey, College of Asia and the Pacific, ANU | en_AU |
local.contributor.affiliation | Horne, Dylan, University of New South Wales | en_AU |
local.contributor.affiliation | Kamminga, Johan, College of Asia and the Pacific, ANU | en_AU |
local.contributor.affiliation | Williams, Alan N., University of New South Wales | en_AU |
local.contributor.authoremail | u7800042@anu.edu.au | en_AU |
local.contributor.authoruid | Hope, Geoffrey, u7800042 | en_AU |
local.contributor.authoruid | Kamminga, Johan, u1809488 | en_AU |
local.description.embargo | 2099-12-31 | |
local.description.notes | Imported from ARIES | en_AU |
local.identifier.absfor | 040300 - GEOLOGY | en_AU |
local.identifier.absfor | 040600 - PHYSICAL GEOGRAPHY AND ENVIRONMENTAL GEOSCIENCE | en_AU |
local.identifier.absfor | 210100 - ARCHAEOLOGY | en_AU |
local.identifier.ariespublication | a383154xPUB14755 | en_AU |
local.identifier.citationvolume | 30 | en_AU |
local.identifier.doi | 10.1177/0959683620941067 | en_AU |
local.identifier.uidSubmittedBy | a383154 | en_AU |
local.publisher.url | https://journals.sagepub.com/ | en_AU |
local.type.status | Published Version | en_AU |
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