thumbnail

Neoproterozoic diamictite-cap carbonate succession and ??13C chemostratigraphy from eastern Sonora, Mexico

Chemical Geology

By:
, ,
DOI: 10.1016/j.chemgeo.2006.06.020

Links

Abstract

Despite the occurrence of Neoproterozoic strata throughout the southwestern U.S. and Sonora, Mexico, glacial units overlain by enigmatic cap carbonates have not been well-documented south of Death Valley, California. Here, we describe in detail the first glaciogenic diamictite and cap carbonate succession from Mexico, found in the Cerro Las Bolas Group. The diamictite is exposed near Sahuaripa, Sonora, and is overlain by a 5??m thick very finely-laminated dolostone with soft sediment folds. Carbon isotopic chemostratigraphy of the finely-laminated dolostone reveals a negative ??13C anomaly (down to - 3.2??? PDB) characteristic of cap carbonates worldwide. Carbon isotopic values rise to + 10??? across ??? 400??m of section in overlying carbonates of the Mina el Mezquite and Monteso Formations. The pattern recorded here is mostly characteristic of post-Sturtian (ca. ??? 700??Ma), but pre-Marinoan (ca. ??? 635??Ma) time. However, the Cerro Las Bolas Group shares ambiguity common to most Neoproterozoic successions: it lacks useful radiometric age constraints and biostratigraphically useful fossils, and its ??13C signature is oscillatory and therefore somewhat equivocal. ?? 2006 Elsevier B.V. All rights reserved.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Neoproterozoic diamictite-cap carbonate succession and ??13C chemostratigraphy from eastern Sonora, Mexico
Series title:
Chemical Geology
DOI:
10.1016/j.chemgeo.2006.06.020
Volume
237
Issue:
1-2
Year Published:
2007
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Chemical Geology
First page:
147
Last page:
160
Number of Pages:
14