Articles | Volume 20, issue 3
Research article
22 Mar 2024
Research article |  | 22 Mar 2024

Weathering trends in the Norian through geochemical and rock magnetic analyses from the Pignola–Abriola section (Lagonegro Basin, Italy)

Matteo Maron, Tetsuji Onoue, Sara Satolli, Katsuhito Soda, Honami Sato, Giovanni Muttoni, and Manuel Rigo


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on cp-2023-61', Anonymous Referee #1, 08 Nov 2023
    • AC1: 'Reply on RC1', Matteo Maron, 08 Jan 2024
    • AC3: 'Reply on RC1', Matteo Maron, 09 Jan 2024
  • EC1: 'Comment on cp-2023-61', Yves Godderis, 04 Dec 2023
    • AC2: 'Reply on EC1', Matteo Maron, 08 Jan 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish as is (26 Jan 2024) by Yves Godderis
AR by Matteo Maron on behalf of the Authors (02 Feb 2024)  Author's response   Manuscript 
Short summary
For better knowledge of the climate perturbation that occurred in the lattermost part of the Triassic (Norian–Rhaetian), we investigated the geochemical and rock magnetic properties of the limestones of the Pignola–Abriola section (Lagonegro Basin, Italy). Our investigation revealed at least a major episode of enhanced weathering occurring in the late Norian (~217–211 Ma), possibly related to the Cimmerian orogen and/or the northward motion of Pangea across the equatorial humid belt.