FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2167296941> ?p ?o ?g. }

• W2167296941 endingPage "1410" @default.
• W2167296941 startingPage "1392" @default.
• W2167296941 abstract "Abstract Caliche is a fairly widespread pedogenic carbonate that commonly has been used to reconstruct palaeoclimatological conditions. Stable isotopic analyses of three types of caliche nodules from Mission Bay, Texas, provide insights into the values and limitations in palaeoenvironmental interpretations. Soft incipient nodules (type I) and partially lithified chalky nodules (type II), composed of low Mg‐calcite, are in situ pedogenic products in the late Quaternary soils; they represent young to intermediate caliche nodules with no obvious diagenesis and, with constraints, can be used to investigate palaeoenvironmental conditions. The well‐lithified hard nodules (type III) dispersed on the beach and shallow bay exhibit complex shapes, fabrics, mineralogy and geochemical compositions. They are mature nodules that have undergone substantial diagenesis and, therefore, are believed to have lost their initial environmental signatures. The incipient nodules in the presently active grey soil and the older subjacent brown soil display significantly different δ 13 C values, −8·4 and −4·4‰, respectively, which indicates a change in palaeovegetation from C 3 / C 4 mixed to C 3 ‐dominated flora. The δ 13 C values probably reflect a marked climate shift from warm and dry to cool and wet conditions in the middle Holocene. However, in the same grey soil, there is a sub‐set of incipient caliche nodules with δ 13 C values around 0·1‰, which is probably due to the input of localized carbon sources in the soil (e.g. shell fragments). The occurrence of essentially identical nodules appearing from the same modern soil horizon with significantly different δ 13 C values questions the universal reliability of this type of data for palaeoenvironmental interpretation. This study demonstrates that, whereas the stable isotopic compositions of caliche nodules can be used for palaeoenvironmental reconstruction, diagenesis and the influence of localized carbonate sources in the soils could lead to erroneous interpretations." @default.
• W2167296941 created "2016-06-24" @default.
• W2167296941 creator A5026743864 @default.
• W2167296941 creator A5081972473 @default.
• W2167296941 date "2009-07-13" @default.
• W2167296941 modified "2023-09-29" @default.
• W2167296941 title "The genesis of late Quaternary caliche nodules in Mission Bay, Texas: stable isotopic compositions and palaeoenvironmental interpretation" @default.
• W2167296941 cites W1911821986 @default.
• W2167296941 cites W1964868755 @default.
• W2167296941 cites W1968522221 @default.
• W2167296941 cites W1974486815 @default.
• W2167296941 cites W1974966466 @default.
• W2167296941 cites W1978124677 @default.
• W2167296941 cites W1978609102 @default.
• W2167296941 cites W1984868639 @default.
• W2167296941 cites W1990906713 @default.
• W2167296941 cites W1993246513 @default.
• W2167296941 cites W2002115844 @default.
• W2167296941 cites W2005435672 @default.
• W2167296941 cites W2008281306 @default.
• W2167296941 cites W2008295328 @default.
• W2167296941 cites W2010202861 @default.
• W2167296941 cites W2013594359 @default.
• W2167296941 cites W2015882712 @default.
• W2167296941 cites W2017245867 @default.
• W2167296941 cites W2017913935 @default.
• W2167296941 cites W2020362962 @default.
• W2167296941 cites W2022000360 @default.
• W2167296941 cites W2028141898 @default.
• W2167296941 cites W2032675137 @default.
• W2167296941 cites W2039657475 @default.
• W2167296941 cites W2043833676 @default.
• W2167296941 cites W2044952903 @default.
• W2167296941 cites W2055891275 @default.
• W2167296941 cites W2061707464 @default.
• W2167296941 cites W2062156648 @default.
• W2167296941 cites W2067250759 @default.
• W2167296941 cites W2072010825 @default.
• W2167296941 cites W2074218038 @default.
• W2167296941 cites W2082046004 @default.
• W2167296941 cites W2085299338 @default.
• W2167296941 cites W2094899605 @default.
• W2167296941 cites W2125872434 @default.
• W2167296941 cites W2128211605 @default.
• W2167296941 cites W2158619594 @default.
• W2167296941 cites W2158814629 @default.
• W2167296941 cites W2170263043 @default.
• W2167296941 cites W2500634497 @default.
• W2167296941 cites W4235141619 @default.
• W2167296941 doi "https://doi.org/10.1111/j.1365-3091.2008.01039.x" @default.
• W2167296941 hasPublicationYear "2009" @default.
• W2167296941 type Work @default.
• W2167296941 sameAs 2167296941 @default.
• W2167296941 citedByCount "10" @default.
• W2167296941 countsByYear W21672969412014 @default.
• W2167296941 countsByYear W21672969412018 @default.
• W2167296941 countsByYear W21672969412019 @default.
• W2167296941 countsByYear W21672969412020 @default.
• W2167296941 crossrefType "journal-article" @default.
• W2167296941 hasAuthorship W2167296941A5026743864 @default.
• W2167296941 hasAuthorship W2167296941A5081972473 @default.
• W2167296941 hasConcept C111368507 @default.
• W2167296941 hasConcept C115880899 @default.
• W2167296941 hasConcept C120806208 @default.
• W2167296941 hasConcept C127313418 @default.
• W2167296941 hasConcept C130452526 @default.
• W2167296941 hasConcept C151730666 @default.
• W2167296941 hasConcept C159390177 @default.
• W2167296941 hasConcept C159750122 @default.
• W2167296941 hasConcept C160464908 @default.
• W2167296941 hasConcept C164430837 @default.
• W2167296941 hasConcept C17409809 @default.
• W2167296941 hasConcept C184269829 @default.
• W2167296941 hasConcept C191897082 @default.
• W2167296941 hasConcept C192562407 @default.
• W2167296941 hasConcept C2780191791 @default.
• W2167296941 hasConcept C2780659211 @default.
• W2167296941 hasConcept C95869378 @default.
• W2167296941 hasConceptScore W2167296941C111368507 @default.
• W2167296941 hasConceptScore W2167296941C115880899 @default.
• W2167296941 hasConceptScore W2167296941C120806208 @default.
• W2167296941 hasConceptScore W2167296941C127313418 @default.
• W2167296941 hasConceptScore W2167296941C130452526 @default.
• W2167296941 hasConceptScore W2167296941C151730666 @default.
• W2167296941 hasConceptScore W2167296941C159390177 @default.
• W2167296941 hasConceptScore W2167296941C159750122 @default.
• W2167296941 hasConceptScore W2167296941C160464908 @default.
• W2167296941 hasConceptScore W2167296941C164430837 @default.
• W2167296941 hasConceptScore W2167296941C17409809 @default.
• W2167296941 hasConceptScore W2167296941C184269829 @default.
• W2167296941 hasConceptScore W2167296941C191897082 @default.
• W2167296941 hasConceptScore W2167296941C192562407 @default.
• W2167296941 hasConceptScore W2167296941C2780191791 @default.
• W2167296941 hasConceptScore W2167296941C2780659211 @default.
• W2167296941 hasConceptScore W2167296941C95869378 @default.
• W2167296941 hasIssue "5" @default.
• W2167296941 hasLocation W21672969411 @default.
• W2167296941 hasOpenAccess W2167296941 @default.

• next