Sedimentary geochemistry examines the chemical processes and signatures in sediments and sedimentary rocks, from their formation through weathering and transport to their burial and diagenetic transformation. Sediment chemistry records source rock composition (provenance), weathering intensity, redox conditions in the depositional environment, and post-depositional diagenetic modifications. Key tools include major-element weathering indices (CIA, CIW), REE patterns for provenance, redox-sensitive trace elements (Mo, U, V, Re) for paleoenvironmental reconstruction, and stable isotope chemostratigraphy (delta-13C, delta-34S, delta-18O) for global biogeochemical changes. Sedimentary rocks are the archive of Earth's surface conditions through time.
Sedimentary rocks are Earth's memory. They record the chemistry of past oceans, atmospheres, weathering regimes, and biological systems in mineral assemblages, major and trace element concentrations, and isotopic compositions that can be measured billions of years after deposition. Sedimentary geochemistry reads this archive.
Provenance analysis uses immobile elements and their ratios to identify the tectonic setting and lithology of the source terrain. REE patterns (Eu anomaly, LREE/HREE slope), Th/Sc ratios (felsic sources have high Th/Sc), and Cr/Th ratios (mafic sources have high Cr) discriminate between felsic continental, mafic oceanic, and recycled sedimentary sources. These ratios survive weathering, transport, and moderate diagenesis, preserving source information in ancient sediments.
Paleoenvironmental reconstruction relies on elements whose behavior changes dramatically with redox conditions. In modern oceans, Mo, V, Re, and U are dissolved under oxygenated conditions but become insoluble and accumulate in sediments under anoxic or euxinic conditions. By measuring their enrichments in ancient sediments and calibrating against modern analogs (Black Sea, Cariaco Basin), geochemists reconstruct the redox state of past water bodies. The secular record of these elements through Earth history documents major oxygenation events, ocean anoxic events, and the long-term evolution of marine redox chemistry.
Diagenesis -- the chemical and physical changes occurring after deposition -- modifies the primary geochemical signal. Organic matter is microbially degraded through the terminal electron acceptor sequence. Pore waters evolve as minerals dissolve and precipitate. Authigenic minerals (pyrite, siderite, dolomite, glauconite) form in the sediment column. Understanding diagenesis is essential for interpreting primary signals correctly and for recognizing which geochemical proxies survive burial and which are overprinted.