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Ángela Mosquera Giménez1*
Pedro Vélez-Belchí1
Jesús Rivera2
Safo Piñeiro3Noelia Fajar4Verónica Caínzos5
Rosa Balbín3Juan Antonio Jiménez Aparicio3
Carlos Dominguez-Carrió6Jordi Blasco-Ferre6
Marina Carreiro-Silva6
Telmo Morato6
Patricia Puerta3
Covadonga Orejas3- 1Centro Oceanográfico de Canarias, Instituto Español de Oceanografía, Santa Cruz de Tenerife, Spain
- 2Servicios Centrales, Instituto Español de Oceanografía, Madrid, Spain
- 3Centro Oceanográfico de Baleares, Instituto Español de Oceanografía, Palma, Spain
- 4Centro Oceanográfico de a Coruña, Instituto Español de Oceanografía, A Coruña, Spain
- 5IOCAG, Universidad de Las Palmas de Gran Canaria, Instituto de Oceanografiìa y Cambio Global, ULPGC, Unidad Asociada ULPGC-CSIC, Las Palmas de Gran Canaria, Spain
- 6Marine and Environmental Sciences Centre, Centro OKEANOS, Instituto Do Mar, Universidade dos Açores, Horta, Portugal
by Mosquera Giménez, Á., Vélez-Belchí, P., Rivera, J., Piñeiro, S., Fajar, N., Caínzos, V., et al. (2019). Front. Mar. Sci. 6:702. doi: 10.3389/fmars.2019.00702
In the original article, there was a mistake in Figure 14 as published. The gray dashed line mentioned in the legend does not appear in the Figure. The corrected Figure 14 appears below.
FIGURE 14
Figure 14. Vertical profiles representing the abundance of benthic invertebrates averaged in 2 m bins for all phyla (A), porifera (B), and cnidaria (C) in Formigas seamount. The gray dashed line represents the coefficient between the bottom slope and the angle of propagation of the internal waves (γ/c).
The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.
Keywords: seamounts, Mediterranean Outflow Water, Taylor columns/caps, internal waves, cold-water corals
Citation: Mosquera Giménez Á, Vélez-Belchí P, Rivera J, Piñeiro S, Fajar N, Caínzos V, Balbín R, Jiménez Aparicio JA, Dominguez-Carrió C, Blasco-Ferre J, Carreiro-Silva M, Morato T, Puerta P and Orejas C (2021) Corrigendum: Ocean Circulation Over North Atlantic Underwater Features in the Path of the Mediterranean Outflow Water: The Ormonde and Formigas Seamounts, and the Gazul Mud Volcano. Front. Mar. Sci. 8:665980. doi: 10.3389/fmars.2021.665980
Received: 09 February 2021; Accepted: 10 February 2021;
Published: 25 February 2021.
Approved by:
Frontiers Editorial Office, Frontiers Media SA, SwitzerlandCopyright © 2021 Mosquera Giménez, Vélez-Belchí, Rivera, Piñeiro, Fajar, Caínzos, Balbín, Jiménez Aparicio, Dominguez-Carrió, Blasco-Ferre, Carreiro-Silva, Morato, Puerta and Orejas. 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) and the copyright owner(s) 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: Ángela Mosquera Giménez, YW5nZWxhLm1vc3F1ZXJhQGllby5lcw==; YW5nZWxhX21vc3FAaG90bWFpbC5jb20=