FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2109747265> ?p ?o ?g. }

• W2109747265 endingPage "74" @default.
• W2109747265 startingPage "61" @default.
• W2109747265 abstract "Accelerator mass spectrometry and conventional radiocarbon age determinations of organic matter from paleosols indicate that the Brandon Sand Hills area of southern Manitoba has been subjected to recurrent intervals of eolian activity in the past 5000 years. Although precise regional correlations are precluded by dating uncertainties, periods of most notable paleosol development occurred around 2300 to 2000, 1400 to 1000, and 600 to 500 cal yr BP with eolian activity occurring before and after each of these periods. Episodes of eolian activity may correspond to periods of regional drought, whereas paleosols mark periods of increased moisture availability and stabilization by vegetation. The geochemistry of the eolian sands, paleosols and source sediments indicates that partial leaching of carbonates occurs from pedogenesis during humid climatic phases, and that this is probably the primary mechanism of carbonate depletion of eolian sands in this area. Recent trends in sand dune activity from historic aerial photography and early explorers’ accounts indicate that the few active dunes that presently exist have stabilized at a rate of 10–20% per decade, despite several severe droughts in the 20th century. This may be attributed to pre-settlement droughts that were more severe than those in historic times although regional dune stabilization may also be related, in part, to the spread of forest cover in the past few hundred years." @default.
• W2109747265 created "2016-06-24" @default.
• W2109747265 creator A5033816671 @default.
• W2109747265 creator A5034408974 @default.
• W2109747265 creator A5050650226 @default.
• W2109747265 creator A5055336005 @default.
• W2109747265 date "2000-05-01" @default.
• W2109747265 modified "2023-10-17" @default.
• W2109747265 title "Chronology and geochemistry of late Holocene eolian deposits in the Brandon Sand Hills, Manitoba, Canada" @default.
• W2109747265 cites W1488519229 @default.
• W2109747265 cites W1533786698 @default.
• W2109747265 cites W1927648166 @default.
• W2109747265 cites W1977498054 @default.
• W2109747265 cites W1982751035 @default.
• W2109747265 cites W1989977439 @default.
• W2109747265 cites W1993734501 @default.
• W2109747265 cites W2012480063 @default.
• W2109747265 cites W2015208407 @default.
• W2109747265 cites W2016895904 @default.
• W2109747265 cites W2022016076 @default.
• W2109747265 cites W2029225949 @default.
• W2109747265 cites W2035015442 @default.
• W2109747265 cites W2035975742 @default.
• W2109747265 cites W2039802288 @default.
• W2109747265 cites W2043392633 @default.
• W2109747265 cites W2044650517 @default.
• W2109747265 cites W2051001115 @default.
• W2109747265 cites W2055136587 @default.
• W2109747265 cites W2059995004 @default.
• W2109747265 cites W2061841731 @default.
• W2109747265 cites W2067890752 @default.
• W2109747265 cites W2069004915 @default.
• W2109747265 cites W2087757302 @default.
• W2109747265 cites W2090127774 @default.
• W2109747265 cites W2120434692 @default.
• W2109747265 cites W2120932199 @default.
• W2109747265 cites W2135613291 @default.
• W2109747265 cites W2138779124 @default.
• W2109747265 cites W2156802280 @default.
• W2109747265 cites W2165085169 @default.
• W2109747265 cites W2280624662 @default.
• W2109747265 cites W248333565 @default.
• W2109747265 cites W2499877093 @default.
• W2109747265 cites W2554647577 @default.
• W2109747265 cites W2909104754 @default.
• W2109747265 cites W2909433998 @default.
• W2109747265 cites W2909482553 @default.
• W2109747265 cites W2910474244 @default.
• W2109747265 cites W2910954275 @default.
• W2109747265 doi "https://doi.org/10.1016/s1040-6182(00)00009-4" @default.
• W2109747265 hasPublicationYear "2000" @default.
• W2109747265 type Work @default.
• W2109747265 sameAs 2109747265 @default.
• W2109747265 citedByCount "76" @default.
• W2109747265 countsByYear W21097472652012 @default.
• W2109747265 countsByYear W21097472652013 @default.
• W2109747265 countsByYear W21097472652014 @default.
• W2109747265 countsByYear W21097472652015 @default.
• W2109747265 countsByYear W21097472652016 @default.
• W2109747265 countsByYear W21097472652017 @default.
• W2109747265 countsByYear W21097472652019 @default.
• W2109747265 countsByYear W21097472652020 @default.
• W2109747265 countsByYear W21097472652021 @default.
• W2109747265 countsByYear W21097472652022 @default.
• W2109747265 countsByYear W21097472652023 @default.
• W2109747265 crossrefType "journal-article" @default.
• W2109747265 hasAuthorship W2109747265A5033816671 @default.
• W2109747265 hasAuthorship W2109747265A5034408974 @default.
• W2109747265 hasAuthorship W2109747265A5050650226 @default.
• W2109747265 hasAuthorship W2109747265A5055336005 @default.
• W2109747265 hasBestOaLocation W21097472652 @default.
• W2109747265 hasConcept C100134115 @default.
• W2109747265 hasConcept C100970517 @default.
• W2109747265 hasConcept C127313418 @default.
• W2109747265 hasConcept C140345934 @default.
• W2109747265 hasConcept C151730666 @default.
• W2109747265 hasConcept C159390177 @default.
• W2109747265 hasConcept C159750122 @default.
• W2109747265 hasConcept C166957645 @default.
• W2109747265 hasConcept C17409809 @default.
• W2109747265 hasConcept C180093795 @default.
• W2109747265 hasConcept C181536285 @default.
• W2109747265 hasConcept C184269829 @default.
• W2109747265 hasConcept C185515318 @default.
• W2109747265 hasConcept C191897082 @default.
• W2109747265 hasConcept C192562407 @default.
• W2109747265 hasConcept C205649164 @default.
• W2109747265 hasConcept C2780659211 @default.
• W2109747265 hasConcept C76123530 @default.
• W2109747265 hasConceptScore W2109747265C100134115 @default.
• W2109747265 hasConceptScore W2109747265C100970517 @default.
• W2109747265 hasConceptScore W2109747265C127313418 @default.
• W2109747265 hasConceptScore W2109747265C140345934 @default.
• W2109747265 hasConceptScore W2109747265C151730666 @default.
• W2109747265 hasConceptScore W2109747265C159390177 @default.
• W2109747265 hasConceptScore W2109747265C159750122 @default.
• W2109747265 hasConceptScore W2109747265C166957645 @default.
• W2109747265 hasConceptScore W2109747265C17409809 @default.

• next