%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Guo, M. E.
%A Alexandre, A.
%A Longstaffe, F. J.
%A Peugeot, Christophe
%A Webb, E. A.
%T 17O-excess of grass leaf phytoliths across the North American prairies records late-growing season daytime relative humidity
%D 2025
%L fdi:010092600
%G ENG
%J Chemical Geology
%@ 0009-2541
%K Phytoliths ; Relative Humidity ; Transpiration ; North American prairies ; O-17-excess
%K AMERIQUE DU NORD
%M ISI:001396977900001
%P 122484 [11 ]
%R 10.1016/j.chemgeo.2024.122484
%U https://www.documentation.ird.fr/hor/fdi:010092600
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2025-02/010092600.pdf
%V 671
%W Horizon (IRD)
%X Because it is an important climate parameter, an accurate proxy is required for the reconstruction of past Relative Humidity (RH). Triple oxygen isotopes of grass-leaf phytoliths have a high potential for this purpose. A strong correlation between RH and O-17-excess of grass leaf phytoliths has been previously demonstrated from calibration experiments in growth chambers and at natural Sub-Saharan African and Mediterranean sites. Here we focus on the potential of 17 O-excess of grass leaf phytoliths as a proxy of RH across the North American Great Plains. We tested the relationship between the O-17-excess of naturally grown Calamovilfa longifolia phytoliths and RH for different periods of the grass growing season. The results show that O-17-excess of leaf phytoliths has a strong correlation with late-growing season (July-August) daytime RH, which varies from 29 to 72 % across North America. The correlation can be expressed as: O-17-excess leaf phytoliths = 4.14(+0.47) x RH (%) - 497(+26) (R-2 = 0.85, p-value<0.0001). To use the O-17-excess of bulk phytoliths buried in soils and sediments as a quantitative proxy of past RH, future calibration studies on soil phytoliths are needed to evaluate the contribution of non-transpiring phytoliths. The(17)O-excess of stem water, which was determined by O-17-excess of stem phytoliths, shows similar values to the O-17-excess of precipitation in North America without evaporation, which therefore does not affect the O-17-excess of leaf phytoliths in North America. These results demonstrate that the O-17-excess of phytoliths is a promising proxy for regional growing season RH.
%$ 021 ; 020 ; 076 ; 068