4.2 Article

A sea bottom classification of the Robredo area in the Northern San Jorge Gulf (Argentina)

期刊

GEO-MARINE LETTERS
卷 41, 期 1, 页码 -

出版社

SPRINGER
DOI: 10.1007/s00367-020-00682-4

关键词

Benthic geohabitat; Multibeam echosounder; Seabed classification; Patagonian Gulf

资金

  1. Ministerio de Ciencia, Tecnologia e Innovacion Productiva (MINCyT)
  2. Provincia de Chubut
  3. Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)

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The study discusses the factors influencing benthic habitats and the research methods used, emphasizing the importance of multibeam echosounders in providing data for seabed classification. The data acquired in the Robredo area reveals the substrate characteristics and bottom structure complexity, leading to important insights into the benthic geohabitats. The results show that Robredo has two subareas with different substrate types, indicating the significance of bottom structure complexity in seabed classification.
Benthic habitats are primarily determined by the nature of the substrate (i.e., the type of sediment or rock) and by the bathymetry (e.g., light availability, current, or waves exposition) both determining the viability of infaunal organisms. In this sense multibeam (MB) echosounders provide more data about the sea bottom than any other acoustic technique. During the 2014 Argentine-Canadian survey of the RV Coriolis II in the Gulf of San Jorge, MB data were acquired in the area of Robredo, west of the Marine Protected Area (MPA) Parque Interjurisdiccional Marino Costero Patagonia Austral (PIMCPA, Patagonia, Argentine). Acoustic data were affected by acquisition artifacts, so an ad hoc algorithm was required to restore the data. Moreover, during the survey, dredge samples were also acquired where acoustic data suggested changes in substrate properties, and two later scientific surveys acquired video transects of the sea bottom that allowed also a basic classification. A non-supervised classification of the seabed was performed, using a subsampling and voting algorithm, with the acoustic and bathymetric data. The final classification is in agreement with groundtruthing (dredge samples and video transects), showing that bottom structure complexity leads to a meaningful picture of the sea bottom classes in the area. Our results reveal that Robredo has two subareas, one with a fine substrate (west) and another with a coarse substrate (east), the latter being also characterized by outcropping rock formations of marked relief. Despite the small spatial coverage of the survey, the resulting sea bottom classification presented in this paper has described, for the first time, some important features of the benthic geohabitats in the PIMCPA.

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