A Corrigendum on
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
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.
Ángela Mosquera Giménez1*, Pedro Vélez-Belchí1, Jesús Rivera2, Safo Piñeiro3, Noelia Fajar4, Verónica Caínzos5, Rosa Balbín3, Juan Antonio Jiménez Aparicio3, Carlos Dominguez-Carrió6, Jordi Blasco-Ferre6, Marina Carreiro-Silva6, Telmo Morato6, Patricia Puerta3 and 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
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