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Guo M. E., Alexandre A., Longstaffe F. J., Peugeot Christophe, Webb E. A. (2025). 17O-excess of grass leaf phytoliths across the North American prairies records late-growing season daytime relative humidity. Chemical Geology, 671, p. 122484 [11 p.]. ISSN 0009-2541.

Titre du document
17O-excess of grass leaf phytoliths across the North American prairies records late-growing season daytime relative humidity
Année de publication
2025
Type de document
Article référencé dans le Web of Science WOS:001396977900001
Auteurs
Guo M. E., Alexandre A., Longstaffe F. J., Peugeot Christophe, Webb E. A.
Source
Chemical Geology, 2025, 671, p. 122484 [11 p.] ISSN 0009-2541
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.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Sciences du milieu [021] ; Pédologie [068] ; Sciences du monde végétal [076]
Description Géographique
AMERIQUE DU NORD
Localisation
Fonds IRD [F B010092600]
Identifiant IRD
fdi:010092600
Contact