Dnarever wrote on Jun 2
nd, 2018 at 2:14pm:
It is not disagreeing with what has been long known only supporting the current position of temperatures in that era.
Really?
"After the last glaciation ended, global temperatures appear to have peaked around 6000 years ago, called the Holocene Climatic Optimum. The warming appears have been largely localised, concentrated in the northern hemisphere in summer,
and average global temperatures did not exceed those of recent decades by much, if at all."
https://www.newscientist.com/article/dn11647-climate-myths-its-been-far-warmer-i...That is part of the reason why the current state of the climate science is called the "Adjustocene".
There have been claims that no it was cooler, hat it wasn't global.
"Evidence for an early Holocene climatic optimum in the Antarctic deep ice-core record"
https://link.springer.com/article/10.1007/BF00193529"In the far Southern Hemisphere (New Zealand and Antarctica), the warmest period during the Holocene appears to have been roughly 8,000 to 10,500 years ago, immediately following the end of the last ice age.[10][11] By 6,000 years ago, the time normally associated with the Holocene Climatic Optimum in the Northern Hemisphere, they had reached temperatures similar to present ones, and they did not participate in the temperature changes of the north. However, some authors have used the term "Holocene Climatic Optimum" to describe the earlier southern warm period, as well."
https://en.wikipedia.org/wiki/Holocene_climatic_optimumwiki references -
Masson, V.; Vimeux, F.; Jouzel, J.; Morgan, V.; Delmotte, M.; Ciais,P.; Hammer, C.; Johnsen, S.; Lipenkov, V.Y.; Mosley-Thompson, E.; Petit, J.-R.; Steig, E.J.; Stievenard, M.; Vaikmae, R. (2000). "Holocene climate variability in Antarctica based on 11 ice-core isotopic records".
.W. Williams; D.N.T. King; J.-X. Zhao K.D. Collerson (2004). "Speleothem master chronologies: combined Holocene 18O and 13C records from the North Island of New Zealand and their paleoenvironmental interpretation". The Holocene. 14 (2): 194–208. doi:10.1191/0959683604hl676rp.