FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313403831> ?p ?o ?g. }

• W4313403831 endingPage "23" @default.
• W4313403831 startingPage "1" @default.
• W4313403831 abstract "Abstract The fluvial geomorphology and stratigraphy on the middle Snake River at Bancroft Springs, Idaho, provide evidence for numerous episodes of Snake River aggradation and incision since the Bonneville Flood at ca. 18 ka. A suite of seven terraces ranging from 20–1 m above modern bankfull elevation records multiple cut-and-fill cycles during the latest Pleistocene and Holocene in response to local base-level controls, variations in sediment supply, and hydroclimate change. Radiocarbon and luminescence dating show that the ages of fluvial aggradation generally coincide with increased sediment supply and likely wetter hydroclimate during onset of the Younger Dryas stadial (ca. 13.2 ka), deglaciation and termination of the Younger Dryas stadial (ca. 11.3 ka), Early Holocene cooling (ca. 8.8 ka), and Neoglacial (ca. 4.5, 2.9, 1.1 ka). Six intervening periods of incision and channel stability may also reflect either reduced sediment supply, drier hydroclimate, or both. The terrace chronology can be correlated to a variety of local and regional paleoclimate proxy records and corresponds well with periods of continental- and global-scale rapid climate change during the Holocene. The fluvial record demonstrates the geomorphic response and sensitivity of large river systems to changes in hydroclimate variability, which has important implications for inferring paleoenvironmental conditions in the region." @default.
• W4313403831 created "2023-01-06" @default.
• W4313403831 creator A5018483491 @default.
• W4313403831 creator A5024756416 @default.
• W4313403831 creator A5028798822 @default.
• W4313403831 creator A5073176673 @default.
• W4313403831 creator A5084905441 @default.
• W4313403831 date "2022-12-19" @default.
• W4313403831 modified "2023-09-30" @default.
• W4313403831 title "Landscape response to hydroclimate variability shown by the post-Bonneville Flood (ca. 18 ka) fluvial-geomorphic history of the middle Snake River, Idaho, USA" @default.
• W4313403831 cites W1522444130 @default.
• W4313403831 cites W1603383113 @default.
• W4313403831 cites W1810239284 @default.
• W4313403831 cites W1974574238 @default.
• W4313403831 cites W1975710354 @default.
• W4313403831 cites W1975715178 @default.
• W4313403831 cites W1988802410 @default.
• W4313403831 cites W1988898629 @default.
• W4313403831 cites W1989400475 @default.
• W4313403831 cites W1995050144 @default.
• W4313403831 cites W1996152836 @default.
• W4313403831 cites W2008348784 @default.
• W4313403831 cites W2018276130 @default.
• W4313403831 cites W2025048629 @default.
• W4313403831 cites W2026259333 @default.
• W4313403831 cites W2027825487 @default.
• W4313403831 cites W2046343174 @default.
• W4313403831 cites W2049339867 @default.
• W4313403831 cites W2052493774 @default.
• W4313403831 cites W2059175769 @default.
• W4313403831 cites W2063289782 @default.
• W4313403831 cites W2065636616 @default.
• W4313403831 cites W2065732221 @default.
• W4313403831 cites W2072034809 @default.
• W4313403831 cites W2083173974 @default.
• W4313403831 cites W2094408279 @default.
• W4313403831 cites W2109269291 @default.
• W4313403831 cites W2114395183 @default.
• W4313403831 cites W2114614483 @default.
• W4313403831 cites W2114727579 @default.
• W4313403831 cites W2120637384 @default.
• W4313403831 cites W2126531241 @default.
• W4313403831 cites W2136718048 @default.
• W4313403831 cites W2148073932 @default.
• W4313403831 cites W2148946545 @default.
• W4313403831 cites W2156208893 @default.
• W4313403831 cites W2157371970 @default.
• W4313403831 cites W2167880123 @default.
• W4313403831 cites W2280624662 @default.
• W4313403831 cites W2299789319 @default.
• W4313403831 cites W2315184916 @default.
• W4313403831 cites W2341326188 @default.
• W4313403831 cites W2344021595 @default.
• W4313403831 cites W2347069051 @default.
• W4313403831 cites W2496996840 @default.
• W4313403831 cites W2895068436 @default.
• W4313403831 cites W2921680353 @default.
• W4313403831 cites W3015391807 @default.
• W4313403831 cites W3017588526 @default.
• W4313403831 cites W3025256062 @default.
• W4313403831 cites W3042674254 @default.
• W4313403831 cites W3084299839 @default.
• W4313403831 cites W3099342361 @default.
• W4313403831 cites W4205355805 @default.
• W4313403831 cites W4246853971 @default.
• W4313403831 cites W4248306787 @default.
• W4313403831 cites W4252380702 @default.
• W4313403831 cites W617967150 @default.
• W4313403831 doi "https://doi.org/10.1017/qua.2022.60" @default.
• W4313403831 hasPublicationYear "2022" @default.
• W4313403831 type Work @default.
• W4313403831 citedByCount "0" @default.
• W4313403831 crossrefType "journal-article" @default.
• W4313403831 hasAuthorship W4313403831A5018483491 @default.
• W4313403831 hasAuthorship W4313403831A5024756416 @default.
• W4313403831 hasAuthorship W4313403831A5028798822 @default.
• W4313403831 hasAuthorship W4313403831A5073176673 @default.
• W4313403831 hasAuthorship W4313403831A5084905441 @default.
• W4313403831 hasConcept C100134115 @default.
• W4313403831 hasConcept C100970517 @default.
• W4313403831 hasConcept C109007969 @default.
• W4313403831 hasConcept C111368507 @default.
• W4313403831 hasConcept C112959462 @default.
• W4313403831 hasConcept C114793014 @default.
• W4313403831 hasConcept C127313418 @default.
• W4313403831 hasConcept C132651083 @default.
• W4313403831 hasConcept C140345934 @default.
• W4313403831 hasConcept C142614818 @default.
• W4313403831 hasConcept C151730666 @default.
• W4313403831 hasConcept C160464908 @default.
• W4313403831 hasConcept C180705331 @default.
• W4313403831 hasConcept C181536285 @default.
• W4313403831 hasConcept C205649164 @default.
• W4313403831 hasConcept C26099304 @default.
• W4313403831 hasConcept C33683781 @default.
• W4313403831 hasConcept C53570757 @default.
• W4313403831 hasConcept C65814071 @default.
• W4313403831 hasConcept C69823785 @default.

• next