Comment on “A new classification system for mixed (turbidite-contourite) depositional systems: Examples, conceptual models and diagnostic criteria for modern and ancient records” by S. Rodrigues, F.J. Hernández-Molina, M. Fonnesu, E. Miramontes, M. Rebesco, D. C. Campbell [Earth-Science Reviews (2022), https://doi.org/10.1016/j.earscirev.2022.104030]
Introduction
In developing a new classification system for mixed (turbidite-contourite) depositional systems, the first and foremost step is to provide a clear and precise definition of the terms “turbidite”, “contourite”, and “bottom current”, the three basic terms that form the foundation of the paper. Disappointingly, Rodrigues et al. (2021) did not define these three basic terms. Consequently, the entire article is a confusing maze of case studies, figures, and assertions without clarity. In articulating this foundational problem, I have identified specific issues with 14 questions under the following topics: (1) the turbidite problem, (2) the contourite problem, (3) the bottom-current problem, and (4) the seismic geometry vs. process sedimentology problem. Hopefully, the authors would avail this opportunity in providing clarity.
Section snippets
The turbidite problem
The strength of a review article relies on its comprehensive coverage of previous contributions on a given topic that serves as the underpinning to advance new concepts. In this context, basic contributions on turbidites and turbidity currents must include the following contributions:
- 1)
The introduction of the term “turbidite” (Kuenen, 1957).
- 2)
The introduction of the classic turbidite facies model (Bouma, 1962).
- 3)
The theoretical sediment concentration of 9% by volume in typical turbidity currents (
The contourite problem
There are two schools of thought in defining contourites.
- 1.
The original school by Hollister (1967) who introduced the term “contourite”. By his definition, contourites represent the deposits of thermohaline-induced geostrophic contour currents. I follow this original definition.
- 2.
The later school by Lovell and Stow (1981, p. 349) who conclude that “Contourite: a bed deposited significantly reworked by a current that is persistent in time and space and flows along slope in relatively deep water
The bottom-current problem
Southard and Stanley (1976) recognized five types of bottom currents at the shelf.
break based on their origin. These currents are generated by (1) thermohaline differences, (2) wind forces, (3) tidal forces, (4) internal waves, and (5) surface waves. In general, there are four types of deep-water bottom currents (Shanmugam, 2008), namely (1) thermohaline-induced geostrophic bottom currents (i.e., contour currents), (2) wind-driven bottom currents, (3) deep-water tidal bottom currents, and (4)
The seismic geometry vs. process sedimentology problem
The conventional basin-floor fans are believed to be composed of sandy turbidites (Vail et al., 1991). This sequence-stratigraphic concept was based on the belief that mounded seismic geometry with bidirectional downlap are supposed to be the manifestation of sandy turbidites in basin-floor areas. In understanding the relationship between seismic geometry (seismic facies) and depositional facies, Mobil Oil Company undertook a major field study in the early 1990s involving several staff in
Funding
No fundings.
Availability of data and materials
The datasets used during the current study are available from the corresponding author on reasonable.
request.
Authors' contributions
G. Shanmugam drafted and revised the manuscript according to reviewers' comments.
Declaration of Competing Interest
The author declares that he has no competing interests or personal relationships that could have.
appeared to influence this discussion.
Acknowledgements
I thank journal editor Jingping Xu for handling this discussion manuscript. As always, I am grateful to my wife Jean for her general comments.
References (28)
- et al.
Large floating clasts in turbidites: a mechanism for their emplacement
Sediment. Geol.
(1988) 50 years of the turbidite paradigm (1950s_1990s): deep-water processes and facies models -a critical perspective
Mar. Pet. Geol.
(2000)Ten turbidite myths
Earth-Sci. Rev.
(2002)Deep-water bottom currents and their deposits
- et al.
Contourite facies and the facies model
- et al.
Sequence of structures in fine-grained turbidites: comparison of recent deepsea and ancient flysch sediments
Sediment. Geol.
(1980) Auto-suspension of transported sediment
Proc. R. Soc. Lond. Ser. A
(1962)Sedimentology of some Flysch Deposits: A Graphic Approach to Facies Interpretation
(1962)- et al.
How is a turbidite actually deposited?
Sci. Adv.
(2022) Sediment Distribution and Deep Circulation in the Western North Atlantic (Unpublished Ph.D. Dissertation)
(1967)