ORIGINAL RESEARCH article

Front. Earth Sci.

Sec. Marine Geoscience

Volume 13 - 2025 | doi: 10.3389/feart.2025.1527469

Seafloor surficial sediment variability across the abyssal plains of the central and eastern Pacific Ocean

Provisionally accepted
Devin  HarrisonDevin Harrison1,2*Jessica  L KolbuszJessica L Kolbusz2Todd  BondTodd Bond2Catriona  MacdonaldCatriona Macdonald3Yakup  NiyaziYakup Niyazi2Alan  JamiesonAlan Jamieson2Heather  A StewartHeather A Stewart1,2
  • 1Kelpie Geoscience, Edinburgh, United Kingdom
  • 2University of Western Australia, Perth, Western Australia, Australia
  • 3British Geological Survey, The Lyell Centre, Edinburgh, Scotland, United Kingdom

The final, formatted version of the article will be published soon.

Abyssal plains lie at water depths of 3000 to 6000 m and account for 84.7% of the global ocean seafloor. This vast landsystem is believed to be one of the major reservoirs of biodiversity within the deep-sea. However, it is also one of the least explored parts of the ocean due to the logistical challenges of exploring at great depths over vast spatial scales. This work presents the first results of the Trans-Pacific Transit (TPT), a six-leg expedition that collected remote imagery and video footage of the seafloor sediments and substrate habitats of the central and eastern Pacific Ocean. Qualitative analysis of lander footage revealed that the surficial sediment coverage identified during the TPT survey is dominated by calcareous sediments, clays, and radiolarian sediments. The spatial distribution of these sediments is mostly consistent with previously suggested predictive distribution models. In comparison, polymetallic nodules are more pervasive across the Pacific Ocean than previously suggested. Several previously unknown nodule sites have been identified and are predominantly located in the clay-dominated seafloor of the North Pacific Ocean. Some of the newly identified nodule fields are located between 0 to 15 o S in the proximity of French Polynesia. All identified nodule sites within the TPT dataset coincide with reduced rates of sedimentation and lower levels of surface Chlorophyll-a. The TPT expedition provides new insights into the seafloor sediment variability and polymetallic nodule distribution over a vast section of the Pacific Ocean, representing an unprecedented scale for modern surveys.

Keywords: Abyssal Plain1, Polymetallic Nodules2, Pacific Ocean3, Seafloor Sediments4, Freefall Landers5, Spatial Analysis6, Subsea imaging7

Received: 27 Nov 2024; Accepted: 08 Apr 2025.

Copyright: © 2025 Harrison, Kolbusz, Bond, Macdonald, Niyazi, Jamieson and Stewart. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence: Devin Harrison, Kelpie Geoscience, Edinburgh, United Kingdom

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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