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Australian farming systems have an enduring history of crop livestock integration which emerged in the face of high climate variability, infertile soils and variable landscapes.
Paleoclimatic and paleoanthropological research in eastern Africa suggested repeated association of critical events in hominin evolution with the most prolonged intervals of high climate variability.
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Three of the most prolonged intervals of predicted high climate variability are 2.79-2.47 Mand1.12-0.92 Ma, and 1.12-0.92 Ma and they largely overlap with the previously defined periods of the occurrence of large lakes [ 86] as well as with inferred aridity phases based on dust records, paleosol δ13C, and the prevalence of grazing bovids [ 87].
Potts (2013) [ 77] defined eight intervals of predicted high climate variability in the last 5 My and argued that most important events in hominin evolution occurred within these periods.
By e-mail I asked Connolley to offer his view of whether the high climate sensitivity estimates (often referred to as the "long tail" of the range of warming possibilities) still had weight.
At the beginning of the Holocene, high climate seasonality favoured fire expansion in this region, as in many other ecosystems of the northern and southern hemispheres.
But although climate rhetoric has been based on fears of high sensitivity, climate policy has not been.
We examined the availability of optimal ecophysiological parameters in 22 years of high temporal climate data during the flowering and fruiting stage of an epiphytic plant, Spanish Moss, with a hemisphere-wide distribution.
The majority of cladogenic events within T. areolatus appear in the Pleistocene with the last two events dating to a period (< 1 Ma) of high amplitude climate oscillations (Table 2 and Figure 2).
However, the type of astronomical forcing remains elusive, hindered by lack of adequate age controls and a poor understanding of pacing mechanisms of high-frequency climate changes during the middle to late Miocene.
This explanation, however, is biased by the scarcity of high-resolution climate records directly associated with human activity and the lack of refined palaeoecological studies from multi-stratified sites in the area.
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