Matches in SemOpenAlex for { <https://semopenalex.org/work/W2069842257> ?p ?o ?g. }
- W2069842257 endingPage "114" @default.
- W2069842257 startingPage "97" @default.
- W2069842257 abstract "The tropics are the major source of heat and moisture for the Australasian region. Determining the tropics' response over time to changes in climate forcing mechanisms, such as summer insolation, and the effects of relative sea level on exposed continental shelves during the Last Glacial period, is an ongoing process of re-evaluation. We present a synthesis of climate proxy data from tropical Australasia spanning the last 30,000 years that incorporates deep sea core, coral, speleothem, pollen, charcoal and terrestrial sedimentary records.Today, seasonal variability is governed largely by the annual migration of the inter-tropical convergence zone (ITCZ), influencing this region most strongly during the austral summer. However, the position of the ITCZ has varied through time. Towards the end of Marine Isotope Stage (MIS) 3, conditions were far wetter throughout the region, becoming drier first in the south. Universally cooler land and sea-surface temperature (SST) were characteristic of the Last Glacial Maximum, with drier conditions than previously, although episodic wet periods are noted in the fluvial records of northern Australia. The deglacial period saw warming first in the Coral Sea and then the Indonesian seas, with a pause in this trend around the time of the Antarctic Cold Reversal (c. 14.5 ka), coincident with the flooding of the Sunda Shelf. Wetter conditions occurred first in Indonesia around 17 ka and northern Australia after 14 ka. The early Holocene saw a peak in marine SST to the northwest and northeast of Australia. Modern vegetation was first established on Indonesia, then progressively south and eastward to NE Australia. Flores and the Atherton Tablelands show a dry period around 11.6 ka, steadily becoming wetter through the early Holocene. The mid-late Holocene was punctuated by millennial-scale variability, associated with the El Nino-Southern Oscillation; this is evident in the marine, coral, speleothem and pollen records of the region." @default.
- W2069842257 created "2016-06-24" @default.
- W2069842257 creator A5001010378 @default.
- W2069842257 creator A5014678668 @default.
- W2069842257 creator A5016424414 @default.
- W2069842257 creator A5019569708 @default.
- W2069842257 creator A5020825692 @default.
- W2069842257 creator A5025171623 @default.
- W2069842257 creator A5035018620 @default.
- W2069842257 creator A5038734578 @default.
- W2069842257 creator A5041202612 @default.
- W2069842257 creator A5042709382 @default.
- W2069842257 creator A5042864646 @default.
- W2069842257 creator A5044001202 @default.
- W2069842257 creator A5050758571 @default.
- W2069842257 creator A5053729687 @default.
- W2069842257 creator A5053799995 @default.
- W2069842257 creator A5055593151 @default.
- W2069842257 creator A5061315346 @default.
- W2069842257 creator A5079243112 @default.
- W2069842257 creator A5083611410 @default.
- W2069842257 creator A5085699983 @default.
- W2069842257 creator A5086759411 @default.
- W2069842257 date "2013-08-01" @default.
- W2069842257 modified "2023-10-01" @default.
- W2069842257 title "Palaeoenvironmental change in tropical Australasia over the last 30,000 years – a synthesis by the OZ-INTIMATE group" @default.
- W2069842257 cites W1481495313 @default.
- W2069842257 cites W1503002892 @default.
- W2069842257 cites W1511524149 @default.
- W2069842257 cites W1606354317 @default.
- W2069842257 cites W1610266852 @default.
- W2069842257 cites W1618617103 @default.
- W2069842257 cites W1647849839 @default.
- W2069842257 cites W1735505211 @default.
- W2069842257 cites W188807237 @default.
- W2069842257 cites W1965071004 @default.
- W2069842257 cites W1967061419 @default.
- W2069842257 cites W1967122037 @default.
- W2069842257 cites W1967972815 @default.
- W2069842257 cites W1969064907 @default.
- W2069842257 cites W1969905974 @default.
- W2069842257 cites W1974769863 @default.
- W2069842257 cites W1975272496 @default.
- W2069842257 cites W1977201347 @default.
- W2069842257 cites W1980424534 @default.
- W2069842257 cites W1981267808 @default.
- W2069842257 cites W1981733710 @default.
- W2069842257 cites W1982536498 @default.
- W2069842257 cites W1982630646 @default.
- W2069842257 cites W1983065260 @default.
- W2069842257 cites W1983549621 @default.
- W2069842257 cites W1985669309 @default.
- W2069842257 cites W1987137619 @default.
- W2069842257 cites W1987600175 @default.
- W2069842257 cites W1988378253 @default.
- W2069842257 cites W1988413915 @default.
- W2069842257 cites W1988737265 @default.
- W2069842257 cites W1988963026 @default.
- W2069842257 cites W1991263619 @default.
- W2069842257 cites W1991756670 @default.
- W2069842257 cites W1993384972 @default.
- W2069842257 cites W1996171872 @default.
- W2069842257 cites W1996932107 @default.
- W2069842257 cites W1997144852 @default.
- W2069842257 cites W1997469801 @default.
- W2069842257 cites W1997626537 @default.
- W2069842257 cites W1998572667 @default.
- W2069842257 cites W1998723920 @default.
- W2069842257 cites W1999244938 @default.
- W2069842257 cites W2000243025 @default.
- W2069842257 cites W2001267119 @default.
- W2069842257 cites W2001976657 @default.
- W2069842257 cites W2004046381 @default.
- W2069842257 cites W2004456546 @default.
- W2069842257 cites W2005536752 @default.
- W2069842257 cites W2005857817 @default.
- W2069842257 cites W2008290113 @default.
- W2069842257 cites W2011291754 @default.
- W2069842257 cites W2011779899 @default.
- W2069842257 cites W2012982424 @default.
- W2069842257 cites W2015718550 @default.
- W2069842257 cites W2019111332 @default.
- W2069842257 cites W2020150676 @default.
- W2069842257 cites W2021645329 @default.
- W2069842257 cites W2022228658 @default.
- W2069842257 cites W2022976623 @default.
- W2069842257 cites W2023496115 @default.
- W2069842257 cites W2024611051 @default.
- W2069842257 cites W2025376383 @default.
- W2069842257 cites W2027385173 @default.
- W2069842257 cites W2027500823 @default.
- W2069842257 cites W2027948757 @default.
- W2069842257 cites W2028178427 @default.
- W2069842257 cites W2028654937 @default.
- W2069842257 cites W2029470377 @default.
- W2069842257 cites W2029536858 @default.
- W2069842257 cites W2030677867 @default.
- W2069842257 cites W2030784517 @default.