Re: The Climate, Environment and Energy Thread
Reply #45 –
Your trivia master was wrong Thry
This is my bread and butter; you can’t understand Australian archaeology without understanding the climatic context. For example, the sundering of Bass and Torres Straits and the inundation of what is now the continental shelf had profound effects on the first Australians.
Stone artefacts have been found on Mud Islands in Port Phillip Bay. While it is possible that Aboriginal people could have navigated there, it would have been an extremely risky voyage in the watercraft they had. However, recent studies have revealed that Port Phillip Bay was dry land between 1,000 and 2,800 years ago and it would have been possible to walk to what would have been prominent dunes on Port Phillip Plain. The major causes of the drying up of Port Phillip Bay was sand deposits blocking the Heads combined with higher than normal evaporation rates, reflecting a drier climate at that time. Port Phillip Bay as dry land features in the oral histories of the Kulin people of central Victoria.
Technically, there are no “ice ages”, it is a lay term. Climate scientists, geologists, archaeologists, palynologists, etc refer to glacial and inter-glacial periods. As I said previously, glacial equates to ice age and inter-glacial is not an ice age in lay terms.
Looking at it from the perspective of the geological time scale:
The Pleistocene is the most recent period of repeated glaciations. Until recently, glaciations were a feature of the end of the Pliocene Period (the “ice age” was the Plio-Pleistocene) but the beginning of the Pleistocene has been pushed back to 2.58 Ma so that all recent repeated glaciations are within the Pleistocene era. In other words, the Pleistocene is the “ice age”.
The Holocene refers to the last 11,700 years, that is, the time since the end of the last major glacial epoch, the Pleistocene or "ice age." There have been the small scale climate shifts since the commencement of the Holocene, including the "Little Ice Age" between about 1,200 and 1,700 CE, but that was restricted to the northern hemisphere. The defining feature of the Holocene is the relatively stable climate, as opposed to the widely fluctuation climate swings of the Pleistocene. Note that the “Little Ice Age” almost overlaps with the period that Port Phillip Bay was dry land so while it was colder in the northern hemisphere, southern Australia was experiencing higher evaporation rates. That does suggest warmer temperatures but a much larger part of Australia was arid during the Pleistocene as more of the water budget was locked up in ice caps and glaciers.
Where confusion can arise is the grouping together of the Pleistocene and Holocene as the Quaternary Period. Most of the 2.59Ma of the Quaternary Period has been glacial so you could say that we are still in a period of repeated glaciation. Of course, that ignores the fact that Holocene is defined as the period following the repeated glaciation of the Pleistocene.
On top of that is the use of Anthropocene as the most recent geological period. I don’t think that there is agreement on when human activity became the driver of climate and environmental change but it doesn’t necessarily coincide with the Holocene period. Many researchers push the commencement of the Anthropocene back beyond 11,700 years BP that is accepted as the end of the Pleistocene.