Matches in SemOpenAlex for { <https://semopenalex.org/work/W4387142712> ?p ?o ?g. }
- W4387142712 endingPage "111822" @default.
- W4387142712 startingPage "111822" @default.
- W4387142712 abstract "The glacial and vegetation patterns of Patagonia are strongly correlated to the behaviour of the Southern westerly winds (SWWs) with palaeoenvironmental evidence for the behaviour of the SWWs interpreted as past changes in southern hemisphere climate and ocean currents. To fully define shifts in the position and intensity of the SWWs palaeoenvironmental data sets must be generated from climate sensitive proxies with sites located in regions that are responsive to changes in effective moisture. Here we present a c. 15,700 yr-old record from a peat bog at Punta Arenas (53°09′S) which was analysed for pollen, pollen preservation, charcoal and organic content to reconstruct changes in the surrounding vegetation, fire history and mire surface wetness. The peat bog lies in a closed basin and so environmental changes likely reflect changes in effective moisture primarily driven by fluctuations in precipitation. During the Late glacial the landscape was virtually treeless and dominated by cold-tolerant steppe/tundra vegetation. This was followed by substantial vegetation changes as Nothofagus woodland expanded and the local site transitioned from a small lake to a fen and later a raised mire. The Early and Mid-Holocene (11,600–6000 cal a BP) was marked by a period of sustained drier conditions evidenced by reduced pollen preservation and increased fire activity. After c. 4600 cal a BP there was a shift to increased effective moisture superimposed with higher magnitude and higher frequency changes in precipitation. The palaeoenvironmental record presented here is used to better define the nature and timing of latitudinal shifts in the position of the SWWs. Careful interpretation of the Nothofagus pollen signal is required as during drier periods small increases in humidity can drive large woodland responses in the pollen record while during periods of higher humidity the woodland may appear to be unresponsive to climatic changes." @default.
- W4387142712 created "2023-09-29" @default.
- W4387142712 creator A5001565454 @default.
- W4387142712 creator A5011734118 @default.
- W4387142712 creator A5060456983 @default.
- W4387142712 creator A5069025607 @default.
- W4387142712 date "2023-12-01" @default.
- W4387142712 modified "2023-10-05" @default.
- W4387142712 title "Climatic inferences from southern Patagonia (~53°S): A holistic palaeoecological approach to tracking the behaviour of the southern westerly winds" @default.
- W4387142712 cites W1967619905 @default.
- W4387142712 cites W1968016620 @default.
- W4387142712 cites W1970909548 @default.
- W4387142712 cites W1974647795 @default.
- W4387142712 cites W1978730132 @default.
- W4387142712 cites W1991980215 @default.
- W4387142712 cites W1994160326 @default.
- W4387142712 cites W1994664019 @default.
- W4387142712 cites W1995980790 @default.
- W4387142712 cites W1997501796 @default.
- W4387142712 cites W2011730282 @default.
- W4387142712 cites W2011743963 @default.
- W4387142712 cites W2017034749 @default.
- W4387142712 cites W2018031219 @default.
- W4387142712 cites W2029183430 @default.
- W4387142712 cites W2029724660 @default.
- W4387142712 cites W2033327978 @default.
- W4387142712 cites W2037648824 @default.
- W4387142712 cites W2037888432 @default.
- W4387142712 cites W2042476750 @default.
- W4387142712 cites W2050964644 @default.
- W4387142712 cites W2051974673 @default.
- W4387142712 cites W2054275107 @default.
- W4387142712 cites W2056543664 @default.
- W4387142712 cites W2056663995 @default.
- W4387142712 cites W2057750914 @default.
- W4387142712 cites W2057988317 @default.
- W4387142712 cites W2059175769 @default.
- W4387142712 cites W2062530016 @default.
- W4387142712 cites W2064442601 @default.
- W4387142712 cites W2068837187 @default.
- W4387142712 cites W2071931475 @default.
- W4387142712 cites W2083319265 @default.
- W4387142712 cites W2083986366 @default.
- W4387142712 cites W2106324800 @default.
- W4387142712 cites W2114365219 @default.
- W4387142712 cites W2117102444 @default.
- W4387142712 cites W2136320885 @default.
- W4387142712 cites W2140477756 @default.
- W4387142712 cites W2141459972 @default.
- W4387142712 cites W2144189057 @default.
- W4387142712 cites W2147220546 @default.
- W4387142712 cites W2156102187 @default.
- W4387142712 cites W2157053038 @default.
- W4387142712 cites W2168168465 @default.
- W4387142712 cites W2279964187 @default.
- W4387142712 cites W2280624662 @default.
- W4387142712 cites W2285578274 @default.
- W4387142712 cites W2299779758 @default.
- W4387142712 cites W2517936818 @default.
- W4387142712 cites W2551831632 @default.
- W4387142712 cites W2563156368 @default.
- W4387142712 cites W2583800769 @default.
- W4387142712 cites W2614464134 @default.
- W4387142712 cites W2626399639 @default.
- W4387142712 cites W2735057818 @default.
- W4387142712 cites W2749968648 @default.
- W4387142712 cites W2767518326 @default.
- W4387142712 cites W2787009430 @default.
- W4387142712 cites W2796563914 @default.
- W4387142712 cites W2801351350 @default.
- W4387142712 cites W2884098188 @default.
- W4387142712 cites W2884853325 @default.
- W4387142712 cites W2915121985 @default.
- W4387142712 cites W2945662962 @default.
- W4387142712 cites W2946688144 @default.
- W4387142712 cites W2993755961 @default.
- W4387142712 cites W2995851846 @default.
- W4387142712 cites W3048951226 @default.
- W4387142712 cites W3080136306 @default.
- W4387142712 cites W3107827049 @default.
- W4387142712 cites W3191491215 @default.
- W4387142712 cites W4246027503 @default.
- W4387142712 cites W4286449079 @default.
- W4387142712 cites W4306293736 @default.
- W4387142712 cites W4313530463 @default.
- W4387142712 cites W4361290713 @default.
- W4387142712 doi "https://doi.org/10.1016/j.palaeo.2023.111822" @default.
- W4387142712 hasPublicationYear "2023" @default.
- W4387142712 type Work @default.
- W4387142712 citedByCount "0" @default.
- W4387142712 crossrefType "journal-article" @default.
- W4387142712 hasAuthorship W4387142712A5001565454 @default.
- W4387142712 hasAuthorship W4387142712A5011734118 @default.
- W4387142712 hasAuthorship W4387142712A5060456983 @default.
- W4387142712 hasAuthorship W4387142712A5069025607 @default.
- W4387142712 hasConcept C100970517 @default.
- W4387142712 hasConcept C105895522 @default.
- W4387142712 hasConcept C111368507 @default.