TY - JOUR
T1 - Consideration of soil types for the calibration of molecular proxies for soil pH and temperature using global soil datasets and Vietnamese soil profiles
AU - Davtian, Nina
AU - Ménot, Guillemette
AU - Bard, Edouard
AU - Poulenard, Jérôme
AU - Podwojewski, Pascal
N1 - Funding Information:
G.M. thanks Anneke de Rouw and the HYDRARIDE consortium for making this study and the connection with pedologists possible through discussions in the field in Cameroon. Work at CEREGE is supported by ECCOREV FR3098 (project ECCOTEMP) and the Collège de France. N.D. thanks Ecole Normale Supérieure de Lyon for providing salary support. We are grateful to two anonymous reviewers for their constructive suggestions that greatly helped us to considerably improve this manuscript.
Publisher Copyright:
© 2016 Elsevier Ltd
PY - 2016/11/1
Y1 - 2016/11/1
N2 - Distribution of branched glycerol dialkyl glycerol tetraethers (brGDGTs) in soils depends on environmental parameters such as mean annual air temperature (MAAT) and soil pH. MBT′/MBT′5ME (methylation index of branched tetraethers) and CBT/CBT′ (cyclization ratio of branched tetraethers) are ratios based on the relative abundances of brGDGTs. Using these ratios, global and regional/local calibrations have been established using surface soils, but generally without any preliminary study of soil types. In this study, we reconsider global MAAT–pH/brGDGT calibrations by assigning soil types to the 358 components of a composite soil dataset. Additionally, we investigate brGDGT-derived proxies in five well-described soil profiles along an altitudinal transect in the Mount Fan Si Pan National Park, northwestern Vietnam. Our results show that at the global scale, traditional MAAT–pH/brGDGT relationships per soil type are significantly different and that MAAT (and pH) residuals per soil type may differ as well, for example between Alisols and Podzols. This effect persists when 5- and 6-methyl brGDGTs are quantified separately. Moreover, MAAT (and pH) residuals per soil type are generally not clearly reduced, including in Leptosols, in which 6-methyl brGDGTs are present. In the Fan Si Pan transect, MBT′/CBT–MAAT estimates showed no significant deviation from expected MAATs. We find, however, that soil type effect – related to vegetation changes and contrasting soil organic carbon properties – may bias MAAT–pH estimates in the Vietnamese soil transect. Furthermore, soil depth plays a role which differs between the different Fan Si Pan soil profiles, likely determined by soil type and history.
AB - Distribution of branched glycerol dialkyl glycerol tetraethers (brGDGTs) in soils depends on environmental parameters such as mean annual air temperature (MAAT) and soil pH. MBT′/MBT′5ME (methylation index of branched tetraethers) and CBT/CBT′ (cyclization ratio of branched tetraethers) are ratios based on the relative abundances of brGDGTs. Using these ratios, global and regional/local calibrations have been established using surface soils, but generally without any preliminary study of soil types. In this study, we reconsider global MAAT–pH/brGDGT calibrations by assigning soil types to the 358 components of a composite soil dataset. Additionally, we investigate brGDGT-derived proxies in five well-described soil profiles along an altitudinal transect in the Mount Fan Si Pan National Park, northwestern Vietnam. Our results show that at the global scale, traditional MAAT–pH/brGDGT relationships per soil type are significantly different and that MAAT (and pH) residuals per soil type may differ as well, for example between Alisols and Podzols. This effect persists when 5- and 6-methyl brGDGTs are quantified separately. Moreover, MAAT (and pH) residuals per soil type are generally not clearly reduced, including in Leptosols, in which 6-methyl brGDGTs are present. In the Fan Si Pan transect, MBT′/CBT–MAAT estimates showed no significant deviation from expected MAATs. We find, however, that soil type effect – related to vegetation changes and contrasting soil organic carbon properties – may bias MAAT–pH estimates in the Vietnamese soil transect. Furthermore, soil depth plays a role which differs between the different Fan Si Pan soil profiles, likely determined by soil type and history.
KW - brGDGTs
KW - Calibration
KW - pH
KW - Soil
KW - Temperature
UR - http://www.scopus.com/inward/record.url?scp=84988699871&partnerID=8YFLogxK
U2 - 10.1016/j.orggeochem.2016.09.002
DO - 10.1016/j.orggeochem.2016.09.002
M3 - Article
AN - SCOPUS:84988699871
SN - 0146-6380
VL - 101
SP - 140
EP - 153
JO - Organic Geochemistry
JF - Organic Geochemistry
ER -