Extirpations and extinctions: a plant microfossil-based history of the demise of rainforest and wet sclerophyll communities in the Lake George basin, Southern Tablelands of NSW, south-east Australia
Mike Macphail
A D , Brad Pillans B , Geoff Hope A and Dan Clark C
+ Author Affiliations
- Author Affiliations
A Department of Archaeology and Natural History, College of Asia and the Pacific, Australian National University, Canberra, ACT 2601, Australia.
B Research School of Earth Sciences, Australian National University, Canberra, ACT 2601, Australia.
C Geoscience Australia, GPO Box 378, Canberra, ACT 2601, Australia.
D Corresponding author. Email: mike.macphail@anu.edu.au
Australian Journal of Botany 68(3) 208-228 https://doi.org/10.1071/BT19076
Submitted: 15 April 2019 Accepted: 16 February 2020 Published: 30 March 2020
Abstract
Sites recording the extinction or extirpation of tropical–subtropical and cool–cold temperate rainforest genera during the Plio–Pleistocene aridification of Australia are scattered across the continent, with most preserving only partial records from either the Pliocene or Pleistocene. The highland Lake George basin is unique in accumulating sediment over c. 4 Ma although interpretation of the plant microfossil record is complicated by its size (950 km2), neotectonic activity and fluctuating water levels. A comparison of this and other sites confirms (1) the extinction of rainforest at Lake George was part of the retreat of Nothofagus-gymnosperm communities across Australia during the Plio–Pleistocene; (2) communities of warm- and cool-adapted rainforest genera growing under moderately warm-wet conditions in the Late Pliocene to Early Pleistocene have no modern analogues; (3) the final extirpation of rainforest taxa at Lake George occurred during the Middle Pleistocene; and (4) the role of local wildfires is unresolved although topography, and, elsewhere, possibly edaphic factors allowed temperate rainforest genera to persist long after these taxa became extinct or extirpated at low elevations across much of eastern Australia. Araucaria, which is now restricted to the subtropics–tropics in Australia, appears to have survived into Middle Pleistocene time at Lake George, although the reason remains unclear.
Additional keywords: Araucaria, Bungendore Formations, Calabrian, ‘Chibanian’, earliest Pleistocene, Early Pleistocene, Gearys Gap, Gelasian, Late Pliocene, Middle Pleistocene, Nothofagus, Ondyong Point, Piacenzian, Podocarpaceae, Symplocos.
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