Open AccessInfluence of provenance and preservation on the carbon isotope variations of dispersed organic matter in ancient floodplain sediments
Author(s) -
Bataille Clément P.,
Mastalerz Maria,
Tipple Brett J.,
Bowen Gabriel J.
Publication year - 2013
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1002/ggge.20294
Subject(s) - geology , provenance , sedimentary depositional environment , sedimentary rock , isotopes of carbon , organic matter , sedimentary organic matter , pedogenesis , geochemistry , peat , total organic carbon , δ13c , paleontology , structural basin , stable isotope ratio , soil water , environmental chemistry , soil science , chemistry , archaeology , history , organic chemistry , physics , quantum mechanics
Carbon isotope ratios of bulk organic matter in sedimentary rocks (δ 13 C DOM ) are a potential source of paleoenvironmental information in terrestrial stratigraphic sequences. However, insufficient understanding of the range of depositional and post‐depositional controls on δ 13 C DOM values makes interpretations of these data difficult. Here we evaluate the effects of organic matter (OM) provenance and preservation on δ 13 C DOM using records spanning the Paleocene Eocene Thermal Maximum (PETM) in the Bighorn Basin (Wyoming, USA) as a case study . We sampled sedimentary rocks spanning the PETM in two well‐studied locations—Polecat Bench (PB) and Highway 16 (HW16)—in the Bighorn Basin. Independent carbon isotope records from biomarkers and pedogenic carbonates at these sites suggest that local shifts in plant and soil δ 13 C values associated with the PETM CIE were broadly similar and were characterized by an abrupt ∼5‰ decrease followed by a plateau and a eventual return to pre‐PETM δ 13 C values. The δ 13 C DOM records from both sites differ significantly from these reference curves in both amplitude of change and in preserving high‐frequency isotopic fluctuations and large isotopic anomalies superimposed on the general pattern of isotopic change through the CIE. For each location, we separated organo‐mineral fractions (MOM), concentrated macerals from 20 stratigraphic levels and analyzed the carbon isotope ratio (δ 13 C) of each fraction. At both sites the δ 13 C of the fine and coarse MOM differ significantly from each other and from δ 13 C DOM . Concentration‐weighted mixing of these isotopically distinct OM fractions explains high resolution δ 13 C DOM fluctuations but does not explain the large isotopic anomalies observed at both sites. At HW16, we identified two thermally and isotopically distinct populations of macerals interpreted as being indigenous and recycled OM. At this site, one over total organic carbon (1/TOC) values correlate with δ 13 C DOM for pre‐PETM and PETM strata and both relationships converge toward the δ 13 C of recycled OM for low TOC. At PB, macerals display homogeneous thermal maturity, but the proportion of isotopically distinct vitrinite and liptinite varies between facies. Relationships between 1/TOC and δ 13 C DOM are also present within specific stratigraphic intervals at PB, but values do not converge on a single isotopic value across the sampled interval. These observations are consistent with variable mixing of OM fractions having different provenance—mixing of exotic recycled OM at HW16 and locally reworked OM at PB with indigenous “fresh” OM at both sites—and explain the large anomalies observed in the δ 13 C DOM records at both sites. Our findings raise questions about the assumption that OM in ancient sediments is indigenous and dominantly records δ 13 C variations of local plants.