Sm. Pelechaty et al., EVALUATION OF DELTA-C-13 CHEMOSTRATIGRAPHY FOR INTRABASINAL CORRELATION - VENDIAN STRATA OF NORTHEAST SIBERIA, Geological Society of America bulletin, 108(8), 1996, pp. 992-1003
Integrated sedimentologic, stratigraphic, and geochemical (delta(13)C,
delta(18)O, Fe, Mn, and Sr) data from Vendian-Cambrian carbonate-ramp
deposits of the northeast Siberian platform (Olenek uplift and Kharau
lakh Mountains region) are used to constrain primary, time-dependent o
scillations in the carbon isotope record and to evaluate delta(13)C ch
emostratigraphy for high-resolution intrabasinal correlation, The Vend
ian delta(13)C record of northeast Siberia reflects global variations
seen elsewhere by displaying (in ascending order) a strong positive is
otopic shift to values near +6 parts per thousand (herein named the P-
interval), an intermediate interval of relatively little isotopic chan
ge (I-interval), which shows, in some sections, a monotonic decrease i
n delta(13)C from +2 parts per thousand at the base to near 0 parts pe
r thousand at the top, and a negative excursion to approximate to-4 pa
rts per thousand (N-interval) just beneath the Vendian-Cambrian bounda
ry, In addition to secular isotopic shifts, these strata exhibit local
small-scale signals related to intrabasinal variations in subsidence,
erosion, and diagenetic alteration (e.g., degradation of organic matt
er, dolomitization, and hydrothermal and burial effects). These local,
intrabasinal processes, in some cases, have modified both the magnitu
de and form of the primary isotopic excursions, which are used as the
basis for correlation in all studies. Carbon isotope profiles provide
an important method to evaluate intrabasinal variations in subsidence,
erosion, and stratigraphic completeness. These profiles reflect incre
asing subsidence along the platform-to-basin transition, whereas progr
essive truncation of isotopic profiles along this trend illustrate pro
nounced uplift and erosion of ramp strata along unconformity surfaces.