Lithological correction of chemical weathering proxies based on K, Rb, and Mg contents for isolation of orbital signals in clastic sedimentary archives

0531007 - ÚACH 2021 RIV NL eng J - Článek v odborném periodiku
Matys Grygar, Tomáš - Mach, K. - Hron, K. - Fačevicová, K. - Martinez, M. - Zeeden, C. - Schnabl, Petr
Lithological correction of chemical weathering proxies based on K, Rb, and Mg contents for isolation of orbital signals in clastic sedimentary archives.
Sedimentary geology. Roč. 406, AUG (2020), č. článku 105717. ISSN 0037-0738. E-ISSN 1879-0968
Grant CEP: GA ČR(CZ) GA19-01768S; GA ČR(CZ) GA16-00800S
Institucionální podpora: RVO:61388980 ; RVO:67985831
Klíčová slova: Cyclostratigraphy * Geochemistry * Log-ratio methodology * Robust statistics * Stratigraphy * Weathering proxies
Obor OECD: Environmental sciences (social aspects to be 5.7); Geology (GLU-S)
Impakt faktor: 3.397, rok: 2020
Způsob publikování: Open access s časovým embargem

The extraction of palaeoenvironmental (palaeoclimatic) signals from the chemical composition of siliciclastic sediments is valuable for the reconstruction of past environments, particularly in continental basins. Here we test novel weathering proxies, which are less sensitive to lithological control than the previously used raw element ratios K/Al, K/Ti, and K/Rb: (1) local enrichment factors of K/Al, Mg/Al, and K/Rb, i.e., the element ratios corrected for grain size- and matrix composition using local background functions (Al/Si, Fe, and Ca as explanatory variables) and ordinary regression and (2) robust regression residuals of those element ratios based on isometric log-ratio coordinates of the most relevant “lithogenic” elements (Ca, Fe, Rb, Si, Zr) in the chemical composition. Chemical weathering proxies can be obtained from departures of chemical composition of sedimentary profiles from relationships with other chemical elements, in particular those with grain-size control. The resulting weathering proxies were examined for the Miocene deposits from the Most Basin, the Czech Republic, which recorded one of the major warm episodes of the Cenozoic time – the Miocene Climatic Optimum. The performance of weathering proxies has been checked by (1) comparison of individual proposed proxies in one drill core HK930, (2) detailed analysis of orbital signals in the relevant compositional functions in HK930, and (3) lateral correlation of three cores HK930, DU7, and DO565 of the same basin. The novel proxies show lateral stability and orbital signatures of short eccentricity, obliquity, and precession, confirming their usefulness in palaeoenvironmental studies. Corrections for grain-size and carbonate contents should help to isolate climatic content from the weathering proxies, although in the studied sediments it weakened the precession component in the orbital signal, as grain-size proxies and other compositional data also carried orbital signals. We propose to consider these proxy ideas in palaeoclimatic reconstructions based on chemical weathering proxies.
Trvalý link: http://hdl.handle.net/11104/0309774


Vědecká data: ScienceDirect