FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3158179918> ?p ?o ?g. }

• W3158179918 endingPage "110413" @default.
• W3158179918 startingPage "110413" @default.
• W3158179918 abstract "Weakly developed paleosols from two distinct interfluve surfaces of Late Pleistocene age provide excellent keys to high-resolution stratigraphic correlation and may serve to trace large-scale genetic packages (systems tract equivalents) across the continental portion of the Po Basin. Twenty-four paleosol profiles from 17 sediment cores were identified and characterized for bulk-geochemical analysis. X-ray fluorescence data were used to trace the degree of weathering. Paleosols, 0.5–1.5 m thick, are pedogenically altered floodplain deposits, developed over time spans of a few thousand of years and mostly partitioned into A-Bk horizons. The most notable paleosol features are dark, organic-matter-rich and carbonate-free mineral surface horizons (A) that overlie bright calcic horizons (Bk) typified by the accumulation of secondary carbonates in the form of pedogenic nodules. Paleosol profiles exhibit a homogeneous geochemical signature that fingerprints a moderate degree of weathering, with little strike- and dip-oriented variability across the different study localities. Plots of Al-normalized calcification and base loss indices against depth reveal systematic increasing values from intensely altered A horizons to underlying Bk horizons. These trends reflect consistent patterns of Ca translocation from surface horizons deeper into the profile, with significant to almost complete Ca removal from A horizons through leaching and accumulation in Bk horizons. Selected trace element ratios (Ba/Sr, Rb/Sr), redox-sensitive trace elements and Zr contents display opposite, up-profile increasing trends that reflect Sr loss in A horizons, with selective Zr concentration in residual minerals. Vertical trends in element ratios are laterally extensive and consistent on a regional basis and represent key pedochemical/stratigraphic markers that can be traced over great distances (tens of kms) throughout the inland portion of the basin. Through quantitative assessment of the degree of weathering, geochemical profiling provides high potential for robust subsurface paleosol correlation that might not be captured by visual core descriptions alone." @default.
• W3158179918 created "2021-05-10" @default.
• W3158179918 creator A5001733693 @default.
• W3158179918 creator A5017598913 @default.
• W3158179918 creator A5019005276 @default.
• W3158179918 creator A5029976905 @default.
• W3158179918 creator A5067358918 @default.
• W3158179918 date "2021-07-01" @default.
• W3158179918 modified "2023-10-17" @default.
• W3158179918 title "Patterns of geochemical variability across weakly developed paleosol profiles and their role as regional stratigraphic markers (Upper Pleistocene, Po Plain)" @default.
• W3158179918 cites W1484202893 @default.
• W3158179918 cites W1547999114 @default.
• W3158179918 cites W1855402894 @default.
• W3158179918 cites W1964275193 @default.
• W3158179918 cites W1974288798 @default.
• W3158179918 cites W1977015349 @default.
• W3158179918 cites W1979384525 @default.
• W3158179918 cites W1980938511 @default.
• W3158179918 cites W1986760631 @default.
• W3158179918 cites W1997749013 @default.
• W3158179918 cites W2002736586 @default.
• W3158179918 cites W2005682761 @default.
• W3158179918 cites W2010056123 @default.
• W3158179918 cites W2012766333 @default.
• W3158179918 cites W2025104665 @default.
• W3158179918 cites W2027192750 @default.
• W3158179918 cites W2028436359 @default.
• W3158179918 cites W2029401070 @default.
• W3158179918 cites W2029828690 @default.
• W3158179918 cites W2030713760 @default.
• W3158179918 cites W2031525304 @default.
• W3158179918 cites W2031795031 @default.
• W3158179918 cites W2037703975 @default.
• W3158179918 cites W2038413411 @default.
• W3158179918 cites W2038739113 @default.
• W3158179918 cites W2055909881 @default.
• W3158179918 cites W2057360759 @default.
• W3158179918 cites W2060605363 @default.
• W3158179918 cites W2060979021 @default.
• W3158179918 cites W2061870593 @default.
• W3158179918 cites W2064051971 @default.
• W3158179918 cites W2065505256 @default.
• W3158179918 cites W2067086897 @default.
• W3158179918 cites W2067250759 @default.
• W3158179918 cites W2074004306 @default.
• W3158179918 cites W2077812289 @default.
• W3158179918 cites W2079891823 @default.
• W3158179918 cites W2082354735 @default.
• W3158179918 cites W2083304964 @default.
• W3158179918 cites W2089502158 @default.
• W3158179918 cites W2095118773 @default.
• W3158179918 cites W2101516930 @default.
• W3158179918 cites W2104224684 @default.
• W3158179918 cites W2122014250 @default.
• W3158179918 cites W2127201634 @default.
• W3158179918 cites W2128142061 @default.
• W3158179918 cites W2131267881 @default.
• W3158179918 cites W2131272880 @default.
• W3158179918 cites W2137875006 @default.
• W3158179918 cites W2138659760 @default.
• W3158179918 cites W2139950654 @default.
• W3158179918 cites W2143989628 @default.
• W3158179918 cites W2160672924 @default.
• W3158179918 cites W2164728255 @default.
• W3158179918 cites W2171586843 @default.
• W3158179918 cites W2219016031 @default.
• W3158179918 cites W2339189462 @default.
• W3158179918 cites W2553988397 @default.
• W3158179918 cites W2582389633 @default.
• W3158179918 cites W2604549016 @default.
• W3158179918 cites W2742849259 @default.
• W3158179918 cites W2758509947 @default.
• W3158179918 cites W2767923635 @default.
• W3158179918 cites W2789687080 @default.
• W3158179918 cites W2803366303 @default.
• W3158179918 cites W2807407651 @default.
• W3158179918 cites W2884417368 @default.
• W3158179918 cites W2893825934 @default.
• W3158179918 cites W2910024282 @default.
• W3158179918 cites W2916935878 @default.
• W3158179918 cites W2944877484 @default.
• W3158179918 cites W3004688477 @default.
• W3158179918 cites W3016752541 @default.
• W3158179918 cites W3044238699 @default.
• W3158179918 cites W3084380204 @default.
• W3158179918 cites W3092283428 @default.
• W3158179918 cites W758298156 @default.
• W3158179918 doi "https://doi.org/10.1016/j.palaeo.2021.110413" @default.
• W3158179918 hasPublicationYear "2021" @default.
• W3158179918 type Work @default.
• W3158179918 sameAs 3158179918 @default.
• W3158179918 citedByCount "8" @default.
• W3158179918 countsByYear W31581799182021 @default.
• W3158179918 countsByYear W31581799182022 @default.
• W3158179918 countsByYear W31581799182023 @default.
• W3158179918 crossrefType "journal-article" @default.
• W3158179918 hasAuthorship W3158179918A5001733693 @default.
• W3158179918 hasAuthorship W3158179918A5017598913 @default.

• next