Elise G. Pendall

Ph.D 1997

 

Prof. Elise Pendall
Ecosystem Ecologist
Department of Botany
University of Wyoming
Laramie, WY 82071
E-mail: pendall@uwyo.edu
Web: http://www.uwyo.edu/terra/ http://uwadmnweb.uwyo.edu/botany/pendall.htm


Ph.D Dissertation Title:Precipitation Seasonality Recorded In D/H Ratios Of Pinyon Pine Cellulose In The Southwestern United States (see Abstract below)

 

 


PRECIPITATION SEASONALITY RECORDED IN D/H RATIOS OF PINYON PINE
CELLULOSE IN THE SOUTHWESTERN UNITED STATES

Department of Geosciences
The University of Arizona
1997

ABSTRACT

I assessed the paleoclimatic significance of dD values of piņon pine (Pinus edulis and P. monophylla) cellulose nitrate (cn) by developing, testing and applying deterministic and empirical models, in the context of the soil-plant-atmosphere continuum. Stable isotope values of precipitaion, soil water, xylem sap, leaf water, atmospheric vapor, annual and sub-annual samples of tree-ring and needle cellulose, and climatic parameters, were measured along a gradient of decreasing summer rain in the southwestern U.S. Stable isotope composition of sap indicated depth of moisture extraction. Over the growing season in New Mexico and Arizona, where monsoon rains are important, trees shifted their water use to shallower depths. In Nevada, where summer rain is scarce, trees shifted to deeper moisture late in the growing season. Evaporation altered dD and d18O values of precipitation inputs to soil. Only after heavy monsoons did soil water and sap isotopically resemble recent precipitation. Average precipitation dD values set the baseline for dDcn values at each site, but interannual variations in relative humidity and precipitation amount altered wood and leaf dDcn values, via leaf water effects. Leaf water (lw) was evaporatively enriched by seasonal moisture stress. dDlw and d18Olw values were strongly correlated with relative humidity on a seasonal basis, but not on a diurnal basis. Measured d18Olw values fit a steady-state model, with an offset attributable to relative humidity. Measured dDlw values were more depleted than predicted by the model, suggesting leaf water-organic matter isotopic exchange. Biochemical fractionation (eB) of hydrogen isotopes between leaf water and cellulose was inversely correlated with relative humidity. Empirical models based on linear regressions demonstrated significant correlations between dDcn values and precipitation seasonality. An El Niņo-Southern Oscillation signal (wood dDcn values inversely related to winter precipitation amount) was found in New Mexico and Arizona. A summer rain signal (leaf dDcn values inversely related to summer humidity) was found at all sites. dDcn values of piņon needles in packrat middens from Sevilleta LTER, New Mexico, suggest that late Pleistocene summers were as wet as today's, and/or that storm tracks could have shifted, bringing in more tropical moisture than currently.