Hardened faecal pellets as a significant component in deep water, subtropical marine environments
Abstract Non‐skeletal carbonate grains are classically interpreted to form in shallow, tropical environments. Peloids deposited in deep, subtropical marine conditions are poorly studied. IODP site U1460 on the subtropical Carnarvon Ramp (Southwest Shelf of Australia) recovered a nearly continuous Pl...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Wiley
2019-06-01
|
Series: | The Depositional Record |
Subjects: | |
Online Access: | https://doi.org/10.1002/dep2.64 |