FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2327661892> ?p ?o ?g. }

• W2327661892 endingPage "8755" @default.
• W2327661892 startingPage "8748" @default.
• W2327661892 abstract "We examined dated sediment cores from 14 thermokarst affected lakes in the Mackenzie Delta uplands, NT, Arctic Canada, using a case-control analysis to determine how retrogressive thaw slump development from degrading permafrost affected the delivery of mercury (Hg) and organic carbon (OC) to lakes. We show that sediments from the lakes with retrogressive thaw slump development on their shorelines (slump-affected lakes) had higher sedimentation rates and lower total Hg (THg), methyl mercury (MeHg), and lower organic carbon concentrations compared to lakes where thaw slumps were absent (reference lakes). There was no difference in focus-corrected Hg flux to sediments between reference lakes and slump-affected lakes, indicating that the lower sediment Hg concentration in slump-affected lakes was due to dilution by rapid inorganic sedimentation in the slump-affected lakes. Sedimentation rates were inversely correlated with THg concentrations in sediments among the 14 lakes considered, and explained 68% of the variance in THg concentration in surface sediment, further supporting the dilution hypothesis. We observed higher S2 (algal-derived carbon) and particulate organic carbon (POC) concentrations in sediment profiles from reference lakes than in slump lakes, likely because of dilution by inorganic siliciclastic matter in cores from slump-affected lakes. We conclude that retrogressive thaw slump development increases inorganic sedimentation in lakes, and decreases concentrations of organic carbon and associated Hg and MeHg in sediments." @default.
• W2327661892 created "2016-06-24" @default.
• W2327661892 creator A5015081661 @default.
• W2327661892 creator A5016083236 @default.
• W2327661892 creator A5022792297 @default.
• W2327661892 creator A5026343780 @default.
• W2327661892 creator A5036123611 @default.
• W2327661892 creator A5042003457 @default.
• W2327661892 creator A5051969500 @default.
• W2327661892 creator A5054476592 @default.
• W2327661892 creator A5072488851 @default.
• W2327661892 date "2012-08-10" @default.
• W2327661892 modified "2023-10-18" @default.
• W2327661892 title "Spatial and Temporal Assessment of Mercury and Organic Matter in Thermokarst Affected Lakes of the Mackenzie Delta Uplands, NT, Canada" @default.
• W2327661892 cites W1967408289 @default.
• W2327661892 cites W1968050600 @default.
• W2327661892 cites W1968880765 @default.
• W2327661892 cites W1973408975 @default.
• W2327661892 cites W1986516591 @default.
• W2327661892 cites W1988281801 @default.
• W2327661892 cites W1994549497 @default.
• W2327661892 cites W1997288102 @default.
• W2327661892 cites W2001651429 @default.
• W2327661892 cites W2005660624 @default.
• W2327661892 cites W2008429427 @default.
• W2327661892 cites W2030838061 @default.
• W2327661892 cites W2039454587 @default.
• W2327661892 cites W2042994920 @default.
• W2327661892 cites W2044883178 @default.
• W2327661892 cites W2050492015 @default.
• W2327661892 cites W2065137445 @default.
• W2327661892 cites W2067156486 @default.
• W2327661892 cites W2077062201 @default.
• W2327661892 cites W2084340585 @default.
• W2327661892 cites W2107076579 @default.
• W2327661892 cites W2137072275 @default.
• W2327661892 cites W2166693526 @default.
• W2327661892 cites W2314170881 @default.
• W2327661892 cites W2319064356 @default.
• W2327661892 doi "https://doi.org/10.1021/es300798w" @default.
• W2327661892 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/22839429" @default.
• W2327661892 hasPublicationYear "2012" @default.
• W2327661892 type Work @default.
• W2327661892 sameAs 2327661892 @default.
• W2327661892 citedByCount "35" @default.
• W2327661892 countsByYear W23276618922013 @default.
• W2327661892 countsByYear W23276618922014 @default.
• W2327661892 countsByYear W23276618922015 @default.
• W2327661892 countsByYear W23276618922016 @default.
• W2327661892 countsByYear W23276618922017 @default.
• W2327661892 countsByYear W23276618922018 @default.
• W2327661892 countsByYear W23276618922019 @default.
• W2327661892 countsByYear W23276618922020 @default.
• W2327661892 countsByYear W23276618922022 @default.
• W2327661892 countsByYear W23276618922023 @default.
• W2327661892 crossrefType "journal-article" @default.
• W2327661892 hasAuthorship W2327661892A5015081661 @default.
• W2327661892 hasAuthorship W2327661892A5016083236 @default.
• W2327661892 hasAuthorship W2327661892A5022792297 @default.
• W2327661892 hasAuthorship W2327661892A5026343780 @default.
• W2327661892 hasAuthorship W2327661892A5036123611 @default.
• W2327661892 hasAuthorship W2327661892A5042003457 @default.
• W2327661892 hasAuthorship W2327661892A5051969500 @default.
• W2327661892 hasAuthorship W2327661892A5054476592 @default.
• W2327661892 hasAuthorship W2327661892A5072488851 @default.
• W2327661892 hasConcept C107872376 @default.
• W2327661892 hasConcept C111368507 @default.
• W2327661892 hasConcept C114793014 @default.
• W2327661892 hasConcept C121332964 @default.
• W2327661892 hasConcept C127313418 @default.
• W2327661892 hasConcept C15098985 @default.
• W2327661892 hasConcept C158787203 @default.
• W2327661892 hasConcept C166957645 @default.
• W2327661892 hasConcept C178790620 @default.
• W2327661892 hasConcept C185592680 @default.
• W2327661892 hasConcept C187320778 @default.
• W2327661892 hasConcept C18903297 @default.
• W2327661892 hasConcept C199360897 @default.
• W2327661892 hasConcept C2777777548 @default.
• W2327661892 hasConcept C2778343803 @default.
• W2327661892 hasConcept C2780155556 @default.
• W2327661892 hasConcept C2816523 @default.
• W2327661892 hasConcept C29941650 @default.
• W2327661892 hasConcept C36574619 @default.
• W2327661892 hasConcept C39432304 @default.
• W2327661892 hasConcept C41008148 @default.
• W2327661892 hasConcept C45291354 @default.
• W2327661892 hasConcept C48743137 @default.
• W2327661892 hasConcept C518008717 @default.
• W2327661892 hasConcept C523993062 @default.
• W2327661892 hasConcept C76886044 @default.
• W2327661892 hasConcept C86803240 @default.
• W2327661892 hasConcept C95457728 @default.
• W2327661892 hasConcept C96618451 @default.
• W2327661892 hasConcept C97355855 @default.
• W2327661892 hasConceptScore W2327661892C107872376 @default.
• W2327661892 hasConceptScore W2327661892C111368507 @default.
• W2327661892 hasConceptScore W2327661892C114793014 @default.

• next