scispace - formally typeset
P

Pierangelo Clari

Researcher at University of Turin

Publications -  36
Citations -  1320

Pierangelo Clari is an academic researcher from University of Turin. The author has contributed to research in topics: Carbonate & Authigenic. The author has an hindex of 20, co-authored 36 publications receiving 1217 citations.

Papers
More filters
Journal ArticleDOI

Cold seep deposits of Beauvoisin (Oxfordian; southeastern France) and Marmorito (Miocene; northern Italy): microbially induced authigenic carbonates

TL;DR: In this article, the relation of two well-known ancient carbonate deposits to hydrocarbon seepage was confirmed by using isotopic signatures corroborate that archaea were involved in the cycling of seepages-derived organic carbon at the ancient localities.
Journal ArticleDOI

The role of bacteria in the formation of cold seep carbonates: geological evidence from Monferrato (Tertiary, NW Italy)

TL;DR: In this article, the identification and description of fossil evidence of microbial activity in the Monferrato carbonates is described. But the authors focus on the identification of microbial structures represented by pyritic rods and dolomite tubes.
Journal ArticleDOI

Discontinuities in carbonate successions: identification, interpretation and classification of some Italian examples

TL;DR: In this article, a number of integrated criteria (geometry, sedimentology, diagenesis, biostratigraphy) have been proposed to recognize stratigraphic breaks.
Journal ArticleDOI

The record of the Messinian salinity crisis in the Tertiary Piedmont Basin (NW Italy): The Alba section revisited

TL;DR: The Alba succession (Tertiary Piedmont basin, NW Italy) preserves the northernmost record of the Messinian salinity crisis (MSC) and was deposited on the southern margin of a wide wedge-top basin this article.
Journal ArticleDOI

A Miocene Mud Volcano and its Plumbing System: A Chaotic Complex Revisited (Monferrato, NW Italy)

TL;DR: In this paper, the authors presented a well-exposed example of the geological record of the birth, life, and death of a mud volcano, showing that the chimneys were the pathway for the expulsion toward the sea floor of gas-and sediment-charged fluids likely originated from destabilization of methane gas hydrates.