@article{monger_stable_1998,
	title = {Stable carbon and oxygen isotopes in {Quaternary} soil caronates as indicators of ecogeomorphic changes in the northern {Chihuahuan} {Desert}, {USA}},
	volume = {82},
	abstract = {Stable carbon and oxygen isotopes in soil carbonates provide an additional technique for investigating Quaternary ecogeomorphic changes in arid and semiarid regions.  This study presents d$^{\textrm{13}}$C and d$^{\textrm{18}}$O values in surface and buried soils in a Basin and Range region of southern New Mexico and west Texas.  Three landform categories were investigated for their isotopic content:  (1) middle piedmont slopes; (2) a lower piedmont slope and adjacent playa depressions; and (3) an intermontane basin floor.  Soils of the middle piedmont slopes had greatest d$^{\textrm{13}}$C variability, ranging from -0.6‰ in buried soils to -11.1‰ (PDB) in surface soils.  Soils of the basin floor had greatest variability in d$^{\textrm{18}}$O values, ranging from -0.6 ‰ to -7.6‰ (PDB).  Fossil pollen patterns roughly paralled d$^{\textrm{13}}$C shifts, with Cheno-Am pollen exhibiting greatest changes.  Both isotope and pollen data across stratigraphic discontinuities suggest that a conversion from C$_{\textrm{4}}$ grasses to C$_{\textrm{3}}$ desert shrubs accomopanied Holocene erosion.  © 1998 Elsevier Science B.V.},
	journal = {Geoderma},
	author = {Monger, H. C. and Cole, D. R. and Gish, J. W. and Giordano, T. H.},
	year = {1998},
	keywords = {JRN, stable isotopes, soil}
}

{"_id":"NsfADuBjxZoCg97Yu","bibbaseid":"monger-cole-gish-giordano-stablecarbonandoxygenisotopesinquaternarysoilcaronatesasindicatorsofecogeomorphicchangesinthenorthernchihuahuandesertusa-1998","downloads":0,"creationDate":"2018-08-10T13:52:57.840Z","title":"Stable carbon and oxygen isotopes in Quaternary soil caronates as indicators of ecogeomorphic changes in the northern Chihuahuan Desert, USA","author_short":["Monger, H. C.","Cole, D. R.","Gish, J. W.","Giordano, T. H."],"year":1998,"bibtype":"article","biburl":"https://utexas.box.com/shared/static/1aa39ptglchcfuw9c04ozm0pqjlxu4rw.bib","bibdata":{"bibtype":"article","type":"article","title":"Stable carbon and oxygen isotopes in Quaternary soil caronates as indicators of ecogeomorphic changes in the northern Chihuahuan Desert, USA","volume":"82","abstract":"Stable carbon and oxygen isotopes in soil carbonates provide an additional technique for investigating Quaternary ecogeomorphic changes in arid and semiarid regions. This study presents d$^{\\textrm{13}}$C and d$^{\\textrm{18}}$O values in surface and buried soils in a Basin and Range region of southern New Mexico and west Texas. Three landform categories were investigated for their isotopic content: (1) middle piedmont slopes; (2) a lower piedmont slope and adjacent playa depressions; and (3) an intermontane basin floor. Soils of the middle piedmont slopes had greatest d$^{\\textrm{13}}$C variability, ranging from -0.6‰ in buried soils to -11.1‰ (PDB) in surface soils. Soils of the basin floor had greatest variability in d$^{\\textrm{18}}$O values, ranging from -0.6 ‰ to -7.6‰ (PDB). Fossil pollen patterns roughly paralled d$^{\\textrm{13}}$C shifts, with Cheno-Am pollen exhibiting greatest changes. Both isotope and pollen data across stratigraphic discontinuities suggest that a conversion from C$_{\\textrm{4}}$ grasses to C$_{\\textrm{3}}$ desert shrubs accomopanied Holocene erosion. © 1998 Elsevier Science B.V.","journal":"Geoderma","author":[{"propositions":[],"lastnames":["Monger"],"firstnames":["H.","C."],"suffixes":[]},{"propositions":[],"lastnames":["Cole"],"firstnames":["D.","R."],"suffixes":[]},{"propositions":[],"lastnames":["Gish"],"firstnames":["J.","W."],"suffixes":[]},{"propositions":[],"lastnames":["Giordano"],"firstnames":["T.","H."],"suffixes":[]}],"year":"1998","keywords":"JRN, stable isotopes, soil","bibtex":"@article{monger_stable_1998,\n\ttitle = {Stable carbon and oxygen isotopes in {Quaternary} soil caronates as indicators of ecogeomorphic changes in the northern {Chihuahuan} {Desert}, {USA}},\n\tvolume = {82},\n\tabstract = {Stable carbon and oxygen isotopes in soil carbonates provide an additional technique for investigating Quaternary ecogeomorphic changes in arid and semiarid regions. This study presents d$^{\\textrm{13}}$C and d$^{\\textrm{18}}$O values in surface and buried soils in a Basin and Range region of southern New Mexico and west Texas. Three landform categories were investigated for their isotopic content: (1) middle piedmont slopes; (2) a lower piedmont slope and adjacent playa depressions; and (3) an intermontane basin floor. Soils of the middle piedmont slopes had greatest d$^{\\textrm{13}}$C variability, ranging from -0.6‰ in buried soils to -11.1‰ (PDB) in surface soils. Soils of the basin floor had greatest variability in d$^{\\textrm{18}}$O values, ranging from -0.6 ‰ to -7.6‰ (PDB). Fossil pollen patterns roughly paralled d$^{\\textrm{13}}$C shifts, with Cheno-Am pollen exhibiting greatest changes. Both isotope and pollen data across stratigraphic discontinuities suggest that a conversion from C$_{\\textrm{4}}$ grasses to C$_{\\textrm{3}}$ desert shrubs accomopanied Holocene erosion. © 1998 Elsevier Science B.V.},\n\tjournal = {Geoderma},\n\tauthor = {Monger, H. C. and Cole, D. R. and Gish, J. W. and Giordano, T. H.},\n\tyear = {1998},\n\tkeywords = {JRN, stable isotopes, soil}\n}\n\n","author_short":["Monger, H. C.","Cole, D. R.","Gish, J. W.","Giordano, T. H."],"key":"monger_stable_1998","id":"monger_stable_1998","bibbaseid":"monger-cole-gish-giordano-stablecarbonandoxygenisotopesinquaternarysoilcaronatesasindicatorsofecogeomorphicchangesinthenorthernchihuahuandesertusa-1998","role":"author","urls":{},"keyword":["JRN","stable isotopes","soil"],"downloads":0},"search_terms":["stable","carbon","oxygen","isotopes","quaternary","soil","caronates","indicators","ecogeomorphic","changes","northern","chihuahuan","desert","usa","monger","cole","gish","giordano"],"keywords":["jrn","stable isotopes","soil"],"authorIDs":[],"dataSources":["gCjo799mKWJtJmSdX"]}