FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2019690023> ?p ?o ?g. }

• W2019690023 endingPage "35" @default.
• W2019690023 startingPage "25" @default.
• W2019690023 abstract "This study presents a pollen-based reconstruction of the vegetation changes and associated climate variations at the Shaamar eolian-paleosol section in the northern Mongolian Plateau. The semi-quantitative reconstructions of paleovegetation types and temperature and moisture indices show that the vegetation in the Shaamar area was a taiga forest dominated by Picea, Abies, and Pinus sibirica-type between ∼38,000 and ∼30,000 cal. BP when the reconstructed moisture level was the highest of the past ∼38,000 years. The vegetation during the ensuing period from ∼30,000 to ∼23,000 cal. BP was mainly a steppe dominated by Artemisia and Poaceae under low temperature and relatively low moisture conditions. The vegetation during the period from ∼23,000 to ∼10,000 cal. BP varied from a taiga forest, through steppe (dominated by Poaceae), taiga forest and forest steppe, to a taiga forest. The climate was cold and relatively dry in the early phase (∼23,000 to ∼20,000 cal. BP) and warmer and somewhat drier in the later phase (∼19,000 to ∼11,000 cal. BP). The pollen assemblages and the vegetation zonal indices suggest that the vegetation was a forest-steppe during the period from ∼10,000 to ∼3000 cal. BP under rising temperature and low moisture conditions. A taiga forest has dominated the landscape during the past ∼3000 years under cooling and wetting conditions. Comparison of our pollen record with other paleoclimatic records suggests that the climate changes in the northern Mongolian Plateau have been controlled or modulated by ocean-atmospheric coupling dynamics in the North Atlantic region." @default.
• W2019690023 created "2016-06-24" @default.
• W2019690023 creator A5002670794 @default.
• W2019690023 creator A5005009127 @default.
• W2019690023 creator A5042469237 @default.
• W2019690023 creator A5044866776 @default.
• W2019690023 creator A5044935460 @default.
• W2019690023 creator A5046597133 @default.
• W2019690023 creator A5083403495 @default.
• W2019690023 date "2013-10-01" @default.
• W2019690023 modified "2023-09-27" @default.
• W2019690023 title "Vegetation changes and associated climate variations during the past ∼38,000 years reconstructed from the Shaamar eolian-paleosol section, northern Mongolia" @default.
• W2019690023 cites W1654234791 @default.
• W2019690023 cites W1966993777 @default.
• W2019690023 cites W1971723721 @default.
• W2019690023 cites W1974629649 @default.
• W2019690023 cites W1977355907 @default.
• W2019690023 cites W1980825605 @default.
• W2019690023 cites W1985534173 @default.
• W2019690023 cites W1990899433 @default.
• W2019690023 cites W1999745977 @default.
• W2019690023 cites W2000795999 @default.
• W2019690023 cites W2000994950 @default.
• W2019690023 cites W2001072306 @default.
• W2019690023 cites W2001573245 @default.
• W2019690023 cites W2004368161 @default.
• W2019690023 cites W2004438023 @default.
• W2019690023 cites W2004897157 @default.
• W2019690023 cites W2008875043 @default.
• W2019690023 cites W2009720500 @default.
• W2019690023 cites W2011974751 @default.
• W2019690023 cites W2013878295 @default.
• W2019690023 cites W2014688144 @default.
• W2019690023 cites W2017036321 @default.
• W2019690023 cites W2021526318 @default.
• W2019690023 cites W2021682235 @default.
• W2019690023 cites W2027536699 @default.
• W2019690023 cites W2029205312 @default.
• W2019690023 cites W2032356558 @default.
• W2019690023 cites W2033075721 @default.
• W2019690023 cites W2035232595 @default.
• W2019690023 cites W2035476929 @default.
• W2019690023 cites W2040399010 @default.
• W2019690023 cites W2041846619 @default.
• W2019690023 cites W2046649840 @default.
• W2019690023 cites W2047463147 @default.
• W2019690023 cites W2055615694 @default.
• W2019690023 cites W2057752775 @default.
• W2019690023 cites W2072470725 @default.
• W2019690023 cites W2074878831 @default.
• W2019690023 cites W2079927432 @default.
• W2019690023 cites W208347246 @default.
• W2019690023 cites W2085875940 @default.
• W2019690023 cites W2086192317 @default.
• W2019690023 cites W2087331075 @default.
• W2019690023 cites W2090766595 @default.
• W2019690023 cites W2093043845 @default.
• W2019690023 cites W2093954470 @default.
• W2019690023 cites W2094168188 @default.
• W2019690023 cites W2094431815 @default.
• W2019690023 cites W2095925839 @default.
• W2019690023 cites W2100693889 @default.
• W2019690023 cites W2102504757 @default.
• W2019690023 cites W2103737089 @default.
• W2019690023 cites W2114868614 @default.
• W2019690023 cites W2116579855 @default.
• W2019690023 cites W2130745784 @default.
• W2019690023 cites W2140477756 @default.
• W2019690023 cites W2142920268 @default.
• W2019690023 cites W2145460885 @default.
• W2019690023 cites W2146045823 @default.
• W2019690023 cites W2148286558 @default.
• W2019690023 cites W2149010791 @default.
• W2019690023 cites W2156246150 @default.
• W2019690023 cites W4211135859 @default.
• W2019690023 cites W4235440090 @default.
• W2019690023 cites W4248294450 @default.
• W2019690023 cites W4306293736 @default.
• W2019690023 doi "https://doi.org/10.1016/j.quaint.2013.08.037" @default.
• W2019690023 hasPublicationYear "2013" @default.
• W2019690023 type Work @default.
• W2019690023 sameAs 2019690023 @default.
• W2019690023 citedByCount "22" @default.
• W2019690023 countsByYear W20196900232014 @default.
• W2019690023 countsByYear W20196900232016 @default.
• W2019690023 countsByYear W20196900232017 @default.
• W2019690023 countsByYear W20196900232019 @default.
• W2019690023 countsByYear W20196900232020 @default.
• W2019690023 countsByYear W20196900232021 @default.
• W2019690023 countsByYear W20196900232022 @default.
• W2019690023 countsByYear W20196900232023 @default.
• W2019690023 crossrefType "journal-article" @default.
• W2019690023 hasAuthorship W2019690023A5002670794 @default.
• W2019690023 hasAuthorship W2019690023A5005009127 @default.
• W2019690023 hasAuthorship W2019690023A5042469237 @default.
• W2019690023 hasAuthorship W2019690023A5044866776 @default.
• W2019690023 hasAuthorship W2019690023A5044935460 @default.
• W2019690023 hasAuthorship W2019690023A5046597133 @default.

• next