FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2036586475> ?p ?o ?g. }

• W2036586475 endingPage "63" @default.
• W2036586475 startingPage "53" @default.
• W2036586475 abstract "Multi-proxy records (geochemistry, clay mineralogy and paleontology) from three sediment cores from Lake Hovsgol, northwest Mongolia, provide paleoenvironmental changes in continental Asia from the last glacial to the present (during the last 29 cal ka BP). This paper presents the first continuous δ13C and δ18O dataset for ostracod shells (Cytherissa lacustris) from Lake Hovsgol sediments. A positive shift in ostracod δ13C values (from + 0.5‰ to + 3.2‰) began at ca. 21 cal ka BP, and was associated with a decrease in δ13C values of total organic carbon (from − 24.7‰ to − 27.3‰) and an increase in the mass accumulation rate of total organic carbon (MAR-TOC). These results suggest that increased lake productivity led to the 13C-enrichment of dissolved inorganic carbon in Lake Hovsgol. In addition, decreases in clay content and the illite crystallinity index (full width at half maximum of the 10 Å peak) began at ca. 21 cal ka BP, indicating an increase in surface runoff and a change in sources of clastic materials in the watershed. The highest δ18Oostracod values (up to − 4.8‰) at 16–15 cal ka BP indicate the increases in precipitation from the East Asian monsoon. The total pollen amount increased, and Betula, Alnus, and Salix were dominant (up to 53%, 30%, and 6%, respectively) after 16–15 cal ka BP. These findings indicate that broad-leaved trees expanded around Lake Hovsgol. In addition, fossil diatom valves appeared after 16–15 cal ka BP, suggesting climate amelioration, and increased input of soil-derived nutrients and dissolved silica. Between 10 and 5 cal ka BP (Holocene climate optimum), productivity was high in and around the lake (MAR-TOC, up to 47.3 mg/cm2 kyr; MAR-diatoms, up to 14.4 × 108 valves/cm2 kyr; total pollen concentration, up to 9.0 × 105 grains/cm3). Environmental changes during the last 29 kyr in and around Lake Hovsgol are clearly associated with fluctuations in summer insolation and East Asian monsoon intensity." @default.
• W2036586475 created "2016-06-24" @default.
• W2036586475 creator A5008471897 @default.
• W2036586475 creator A5015362706 @default.
• W2036586475 creator A5030674524 @default.
• W2036586475 creator A5031527913 @default.
• W2036586475 creator A5033069416 @default.
• W2036586475 creator A5074929661 @default.
• W2036586475 creator A5074965608 @default.
• W2036586475 date "2012-05-01" @default.
• W2036586475 modified "2023-10-16" @default.
• W2036586475 title "Last glacial to post glacial climate changes in continental Asia inferred from multi-proxy records (geochemistry, clay mineralogy, and paleontology) from Lake Hovsgol, northwest Mongolia" @default.
• W2036586475 cites W1615590725 @default.
• W2036586475 cites W1895888640 @default.
• W2036586475 cites W1966431127 @default.
• W2036586475 cites W1979458497 @default.
• W2036586475 cites W1989972918 @default.
• W2036586475 cites W1994007098 @default.
• W2036586475 cites W1995083616 @default.
• W2036586475 cites W1998605684 @default.
• W2036586475 cites W1999080586 @default.
• W2036586475 cites W2000994950 @default.
• W2036586475 cites W2008003790 @default.
• W2036586475 cites W2013231406 @default.
• W2036586475 cites W2013254818 @default.
• W2036586475 cites W2013428409 @default.
• W2036586475 cites W2019558782 @default.
• W2036586475 cites W2020150439 @default.
• W2036586475 cites W2026654802 @default.
• W2036586475 cites W2027385173 @default.
• W2036586475 cites W2029181822 @default.
• W2036586475 cites W2032356558 @default.
• W2036586475 cites W2035325438 @default.
• W2036586475 cites W2038128466 @default.
• W2036586475 cites W2045600400 @default.
• W2036586475 cites W2047925433 @default.
• W2036586475 cites W2050966311 @default.
• W2036586475 cites W2054113365 @default.
• W2036586475 cites W2055303152 @default.
• W2036586475 cites W2056768744 @default.
• W2036586475 cites W2059226621 @default.
• W2036586475 cites W2060258856 @default.
• W2036586475 cites W2066357268 @default.
• W2036586475 cites W2073553672 @default.
• W2036586475 cites W2078613396 @default.
• W2036586475 cites W2079373580 @default.
• W2036586475 cites W2079619902 @default.
• W2036586475 cites W2083357624 @default.
• W2036586475 cites W2086192317 @default.
• W2036586475 cites W2088878159 @default.
• W2036586475 cites W2093778030 @default.
• W2036586475 cites W2094845748 @default.
• W2036586475 cites W2102939273 @default.
• W2036586475 cites W2115642787 @default.
• W2036586475 cites W2140477756 @default.
• W2036586475 cites W2141459972 @default.
• W2036586475 cites W2145725460 @default.
• W2036586475 cites W2147113208 @default.
• W2036586475 cites W2153542422 @default.
• W2036586475 cites W4211135859 @default.
• W2036586475 cites W4240306559 @default.
• W2036586475 cites W4306293736 @default.
• W2036586475 doi "https://doi.org/10.1016/j.gloplacha.2012.03.005" @default.
• W2036586475 hasPublicationYear "2012" @default.
• W2036586475 type Work @default.
• W2036586475 sameAs 2036586475 @default.
• W2036586475 citedByCount "12" @default.
• W2036586475 countsByYear W20365864752013 @default.
• W2036586475 countsByYear W20365864752014 @default.
• W2036586475 countsByYear W20365864752015 @default.
• W2036586475 countsByYear W20365864752017 @default.
• W2036586475 countsByYear W20365864752020 @default.
• W2036586475 countsByYear W20365864752021 @default.
• W2036586475 crossrefType "journal-article" @default.
• W2036586475 hasAuthorship W2036586475A5008471897 @default.
• W2036586475 hasAuthorship W2036586475A5015362706 @default.
• W2036586475 hasAuthorship W2036586475A5030674524 @default.
• W2036586475 hasAuthorship W2036586475A5031527913 @default.
• W2036586475 hasAuthorship W2036586475A5033069416 @default.
• W2036586475 hasAuthorship W2036586475A5074929661 @default.
• W2036586475 hasAuthorship W2036586475A5074965608 @default.
• W2036586475 hasConcept C100970517 @default.
• W2036586475 hasConcept C107872376 @default.
• W2036586475 hasConcept C111368507 @default.
• W2036586475 hasConcept C121332964 @default.
• W2036586475 hasConcept C127313418 @default.
• W2036586475 hasConcept C132651083 @default.
• W2036586475 hasConcept C151730666 @default.
• W2036586475 hasConcept C156398188 @default.
• W2036586475 hasConcept C15739521 @default.
• W2036586475 hasConcept C158787203 @default.
• W2036586475 hasConcept C17409809 @default.
• W2036586475 hasConcept C185059815 @default.
• W2036586475 hasConcept C185592680 @default.
• W2036586475 hasConcept C188291805 @default.
• W2036586475 hasConcept C205649164 @default.
• W2036586475 hasConcept C22117777 @default.
• W2036586475 hasConcept C2776077807 @default.

• next