FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1983603047> ?p ?o ?g. }

• W1983603047 endingPage "152" @default.
• W1983603047 startingPage "134" @default.
• W1983603047 abstract "The hydrology of western Central Asia is highly sensitive to climatic perturbations. In order to understand its long-term variability and to infer linkages between precipitation and atmospheric and oceanic systems, we conducted a thorough sedimentary and geochemical study on a composite core retrieved in lake Son Kul (central Kyrgyzstan). A multi-proxy approach was conducted on lake sediments based on grain size analyses, magnetic susceptibility, total organic carbon (TOC), total nitrogen (TN) and carbon and oxygen isotope analyses on bulk and biogenic materials (ostracoda and molluscs shells) at a resolution equivalent to ca 40 years, aiming to characterise the sequence of palaeolimnological changes in Son Kul. As indicated by δ18O record of bulk carbonates, mainly consisting of aragonite, the Holocene hydrological balance was negative during most of time, suggesting an excess of evaporation (E) over precipitation (P). Limnological conditions fluctuated rapidly before 5000 cal yr BP indicating significant changes in regional hydrology and climate. In particular, the long-term negative hydrological balance was impeded by several short stages with marked increase of precipitation, lasting several decades to a few centuries (e.g., 8300–8200, 6900–6700, 6300–6100, 5500–5400, 5300–5200 and 3100–3000 cal yr BP). Precipitation changes as inferred from δ18O data are also documented by increased minerogenic detritus and higher TOC. We propose that the seasonal pattern of precipitation varied transiently in western Central Asia during the Holocene, although evaporation changes may also account for the rapid changes observed in δ18O data. When the annual water balance was less critical (P ≤ E), the excess of water might be ascribed to increased precipitation during cold seasons mainly because winter precipitation has more negative δ18O than its summer equivalent. Conversely, when the annual water balance is negative (P ≪ E), the moisture was mainly delivered during the warm season, as between 5000 and 2000 cal yr BP. Our results thus imply that moisture sources could have changed as well during the Holocene. Moisture was delivered as today mainly during summer from the extended Caspian-Aral Basin and eastern Mediterranean, although Arctic and even North Atlantic seas might be important moisture sources when seasonal precipitation was dominated by winter precipitation. We hypothesise that warming Arctic and North Atlantic seas were important for the North Hemisphere circulation during the cold season." @default.
• W1983603047 created "2016-06-24" @default.
• W1983603047 creator A5020219007 @default.
• W1983603047 creator A5022812348 @default.
• W1983603047 creator A5029931758 @default.
• W1983603047 creator A5043161023 @default.
• W1983603047 creator A5052078769 @default.
• W1983603047 creator A5053137892 @default.
• W1983603047 creator A5084687224 @default.
• W1983603047 creator A5086922819 @default.
• W1983603047 date "2014-11-01" @default.
• W1983603047 modified "2023-10-05" @default.
• W1983603047 title "Hydrological changes in western Central Asia (Kyrgyzstan) during the Holocene as inferred from a palaeolimnological study in lake Son Kul" @default.
• W1983603047 cites W1570801260 @default.
• W1983603047 cites W1774412088 @default.
• W1983603047 cites W1963640185 @default.
• W1983603047 cites W1966359065 @default.
• W1983603047 cites W1967168939 @default.
• W1983603047 cites W1971336930 @default.
• W1983603047 cites W1972246531 @default.
• W1983603047 cites W1974121020 @default.
• W1983603047 cites W1976172171 @default.
• W1983603047 cites W1976273764 @default.
• W1983603047 cites W1983700413 @default.
• W1983603047 cites W1984905107 @default.
• W1983603047 cites W1987748614 @default.
• W1983603047 cites W1987983109 @default.
• W1983603047 cites W1989332158 @default.
• W1983603047 cites W1990783861 @default.
• W1983603047 cites W1990899433 @default.
• W1983603047 cites W1991533147 @default.
• W1983603047 cites W1995083616 @default.
• W1983603047 cites W1995825783 @default.
• W1983603047 cites W1996932107 @default.
• W1983603047 cites W1997999838 @default.
• W1983603047 cites W1998969760 @default.
• W1983603047 cites W1999745977 @default.
• W1983603047 cites W2002130972 @default.
• W1983603047 cites W2003409354 @default.
• W1983603047 cites W2003946714 @default.
• W1983603047 cites W2003999641 @default.
• W1983603047 cites W2006778670 @default.
• W1983603047 cites W2008005761 @default.
• W1983603047 cites W2011974751 @default.
• W1983603047 cites W2013428409 @default.
• W1983603047 cites W2014058542 @default.
• W1983603047 cites W2014147919 @default.
• W1983603047 cites W2015906898 @default.
• W1983603047 cites W2017307427 @default.
• W1983603047 cites W2017913935 @default.
• W1983603047 cites W2031333660 @default.
• W1983603047 cites W2031790426 @default.
• W1983603047 cites W2034203033 @default.
• W1983603047 cites W2035476929 @default.
• W1983603047 cites W2036778272 @default.
• W1983603047 cites W2037150764 @default.
• W1983603047 cites W2039003315 @default.
• W1983603047 cites W2041711719 @default.
• W1983603047 cites W2044460144 @default.
• W1983603047 cites W2045099531 @default.
• W1983603047 cites W2046171913 @default.
• W1983603047 cites W2048867112 @default.
• W1983603047 cites W2051295811 @default.
• W1983603047 cites W2051973454 @default.
• W1983603047 cites W2064255917 @default.
• W1983603047 cites W2066636062 @default.
• W1983603047 cites W2067118661 @default.
• W1983603047 cites W2074347427 @default.
• W1983603047 cites W2074833779 @default.
• W1983603047 cites W2075452818 @default.
• W1983603047 cites W2075459166 @default.
• W1983603047 cites W2076592609 @default.
• W1983603047 cites W2077414487 @default.
• W1983603047 cites W2077686034 @default.
• W1983603047 cites W2077849516 @default.
• W1983603047 cites W2082422470 @default.
• W1983603047 cites W2090766595 @default.
• W1983603047 cites W2091256005 @default.
• W1983603047 cites W2091980478 @default.
• W1983603047 cites W2095399378 @default.
• W1983603047 cites W2096484028 @default.
• W1983603047 cites W2101522077 @default.
• W1983603047 cites W2111562164 @default.
• W1983603047 cites W2114415381 @default.
• W1983603047 cites W2124965732 @default.
• W1983603047 cites W2125710531 @default.
• W1983603047 cites W2126111165 @default.
• W1983603047 cites W2130266255 @default.
• W1983603047 cites W2133732249 @default.
• W1983603047 cites W2135356319 @default.
• W1983603047 cites W2135696710 @default.
• W1983603047 cites W2135943018 @default.
• W1983603047 cites W2136246993 @default.
• W1983603047 cites W2141643578 @default.
• W1983603047 cites W2151308353 @default.
• W1983603047 cites W2154282956 @default.
• W1983603047 cites W2154983045 @default.
• W1983603047 cites W2164336439 @default.

• next