Infaunal macrobenthos in the Porcupine Bank (NE Atlantic)

The results of the macroinfaunal communities distributions from the annual series surveys PORCUPINE are shown. Those surveys were realized during the months of September and October in the years 2006, 2008, 2009, 2010, 2011, 2012 and 2013 by the Instituto Español de Oceanografía aboard the R /V Vizconde de Eza, within the research project ERDEM. This survey series has as main objective the obtainment of abundance indexes of the benthonic and demersal fauna from Porcupine Bank, west of Ireland, with special attention on the commercial species exploited by the Spanish fleet (hake, angler fish, megrim and norwegian lobster). For the study of the infaunal macrobenthos a total of 50 samples were analyzed from selected places of the Bank, where the bottom characteristics, the climatology or the survey schedule allowed. Samples were taken with an ULSNER box corer with 0.09 m2 of sampling area. Samples for the faunal study were sieved aboard with a 0.5 mm mesh size sieve. The material collected in the sieve was preserved with 8 % formaldehyde neutralized with borax, and stained with Rose Bengal solution for the posterior sorting and identification of fauna. Additional samples were taken to estimate the organic content of the sediment and to perform the granulometric analyses. Once in the laboratory, the granulometry was analyzed following the method recommended by Buchanan (1984); which consists in a combination of dry sieving of the coarse fraction (> 62 µm) and the sedimentation at 20 ºC of the fine fraction (< 62 µm) in a distilled water column. Sediment organic matter content was calculated as the percentage of weight loss by means of 24 hours sample calcination at 500 ºC, after dried it at 100 ºC during the same time. Complementary, in order to obtain a better coverage of the sedimentary types from the study area, more than 350 samples were collected with a net collector coupled to the trawling fishing gear (Baca-GAV 39/52). Globally, the sediments of the majority of the sampled stations are mainly formed by sand, between fine and very fine, except in deep areas of the southeast, where there are large muddy areas with elevated organic content and high selection coefficient. In the north, around the shallowest area, we found thicker sandy sediments, with lower organic content and moderate selection. The macroinfaunal communities from the Porcupine Bank are characterized by the dominance of the faunistic group of polychaetes (68.8 %), mainly represented by the families Owenidae, Spionidae, Paraonidae and Sabellidae. The next in number are the group of molluscs (17.6 %), dominated by the family Kelliellidae, which reaches maximum abundances up to 7520 ind•m-2. The poorest represented groups are the crustaceans (5.0 %), echinoderms (4.3 %) and the “others” (sipunculids, nemertine, etc.), being the latter the least abundant (3.7 %). In relation with the spatial distribution four macroinfaunal groups were indentified in the Porcupine Bank: - Group 1: located in intermediate depth areas, over sandy sediments with low organic content. The infaunal community is dominated by polychaetes from the Owenidae family, mainly represented by the specie Galathowenia oculata. - Group 2: occupies the sandy and low organic content sediments from the shallowest area of the Bank. Polychaetes are the most representative faunistic group, highlighting the dominance of the families Spionidae and Paraonidae. Prionospio fallax and Aricidea wassi are the most representative species of the group. - Group 3: situated in two deep areas in the south area of the Bank with muddy and high organic matter content sediments. It has the lowest infaunal abundance of the study, being dominated by the bivalve molluscs from the family Kelliellidae and by the annelids polychaetes from the family Paraonidae. - Group 4: Is the cluster that includes more stations in throughout the study. It is distributed spatially in the south area of the Bank, in different bathymetries, with the most heterogeneous sediments and moderate organic content. The bivalve molluscs from the Kelliellidae family again become dominant, with Kelliella miliaris reaching abundance over 7500 ind•m-2.IE

Epibenthic communities of sedimentary habitats in a NE Atlantic deep seamount (Galicia Bank)

En prens

Caracterización ecológica del área marina del banco de Galicia

Se integra información hidrográfica, geomorfológica, sedimentológica, biológica, sobre hábitats marinos y pesquera, para establecer las bases ecológicas necesarias para la protección y conservación del banco de GaliciaEl banco de Galicia es un monte submarino profundo situado a 180 km de la costa gallega, con una cima situada entre los 650 y los 1.500 m de profundidad y rodeado de zonas abisales de más de 4.000 m de profundidad. El relieve de las montañas submarinas interactúa con la circulación oceánica modificando las condiciones de oligotrofismo imperantes en el mar profundo. El cambio de dirección de las corrientes marinas, al chocar con el banco, produce las llamadas columnas de Taylor que tienen como consecuencia giros sobre la cima y finalmente un enriquecimiento de las aguas que bañan el banco, lo que influye, a través de la cadena trófica, en las especies de cetáceos, aves y tortugas. Estas condiciones, junto al aislamiento de estos bancos, convierten a estos bancos en puntos calientes de biodiversidad. Esta teoría se ha visto corroborada por los estudios realizados en el proyecto INDEMARES, basados en dos campañas de investigación, dónde se ha encontrado una elevada biodiversidad y la presencia de hábitats vulnerables. El banco de Galicia está bañado por tres capas diferentes: la masa de agua central del Atlántico nordeste europeo (East North Atlantic Central Water: ENACW), por debajo de las aguas superficiales y hasta los 500-600 m; la masa de agua mediterránea (Mediterranean Outflow Water: MOW) y la masa de agua del Labrador (Labrador Sea Water: LSW), que es la capa más profunda. En cuanto al tipo de fondo, se encuentra roca en el área del flanco oriental y hacia el sureste y en los montes adyacentes como el Rucabado, distinguiendo claramente dos tipos en cuanto a la pendiente, correspondiendo con la roca plana de la cima y la roca en pendiente del borde del banco y paredes. En la cima se encuentran fondos de arenas medias, de reflectividad media y baja según el espesor de sedimento, y arenas finas en los fondos sedimentaruios de los flancos, a profundidades mayores de 1.500. En el banco se han identificado hasta el momento 793 especies, con taxones que superan las 100 especies como son moluscos, peces (con especial énfasis en los elasmobranquios), crustáceos y cnidarios. Este inventario incluye especies nuevas para la ciencia, primeras citas para aguas españolas y europeas y especies de gran interés científico y biogeográfico. Este último punto se explica por la situación del Banco entre regiones biogeográficas conectadas por corrientes y masas de agua. El estudio de las conexiones tróficas entre este elevado número de especies ha mostrado el reforzamiento de las rutas bentopelágicas (gambas y macrozooplancton) frente a las dietas epi- y endobentónicas más habituales en otros fondos equivalentes. Mediante técnicas de muestreo extractivas (arrastres, dragas) y de vídeo, y su proyección sobre la interpretación geomorfológica realizada a partir de la sonda multihaz, se ha obtenido una estimación de la distribución de los hábitats bentónicos del banco. Los hábitats identificados en fondos sedimentarios son 1) arenas medias con ofiuras Ophiacantidae y Flabellum chunii, 2) arenas medias con arrecife de corales profundos de Lophelia pertusa y/o Madrepora oculata, y 3) arenas finas con holoturias elasipódidas (Benthogone rosea). En fondos rocosos se han caracterizado los hábitats de 4) roca batial sin pendiente con gorgonias y corales negros, 5) roca batial de talud con comunidades de corales y esponjas, 6) roca batial de talud con corales blancos, bambú y negros, gorgonias y esponjas, 7) arrecife de corales profundos de Lophelia pertusa y/o Madrepora oculata y 8) roca con nódulos manganésicos. El único tipo de hábitat de la DH descrito en la zona es el 1.170 (arrecifes). Sólo se han incluido en la Directiva Hábitats como 1.170 aquellos que presentaban una densidad y diversidad suficientes para cumplir la definición de “arrecifes”. De los hábitats descritos en el banco (ver características ecológicas y biológicas más arriba) solo se han incluido en el 1.170 los arrecifes de corales blancos situados en las arenas medias de la cima del banco, los arrecifes de corales blancos de aguas frías de las especies Lophelia pertusa y Madrepora oculata sobre la roca de la cima del monte Rucabado, las comunidades de roca batial de talud de la ladera sur del banco constituidas por colonias de corales blancos de aguas frías de las especies Lophelia pertusa y Madrepora oculata, y una fauna acompañante muy diversa de escleractinias solitarias, corales bambú, corales negros, gorgonias y esponjas de gran porte, y el resto de zonas de roca batial de talud con comunidades de corales y esponjas. Muchos de los hábitats pueden ser incluidos en los listados de hábitat vulnerables de OSPAR, en los tipos jardines de coral, agregaciones de esponjas de profundidad, arrecifes de Lophelia y montículos carbonatados. En cuanto a las especies de interés para la protección, de las citadas en el banco, el delfín mular (Tursiops truncatus) y la tortuga boba (Caretta caretta) son las únicas especies que figuran en el Anexo II de la Directiva de Hábitats. Sin embargo, muchas epecies de elasmobranquis y algunos peces óseos son consideradas vulnerables, amenazadas o en declive según los criterios definidos por OSPAR y la lista roja de especies amenazadas de IUCN. Algunas de están protegidas por el reglamento europeo 1262/2012 que regula la pesca de especies profundas. La lejanía del banco respecto a los principales focos de presión y la ausencia casi total de presión pesquera hace que el grado de conservación sea muy alto, pudiéndose hablar de un ecosistema prácticamente prístino. Las recomendaciones para la gestión de esta zona van encaminadas a garantizar esta calidad ambiental actual.Instituto Español de Oceanografía, Comisión Europea Programa LIFE+, Fundación Biodiversida

Preliminary Results on the Composition and Structure of Soft-Bottom Macrobenthic Communities of a Seamount: the Galicia Bank (NE Atlantic Ocean)

The Galicia Bank (Atlantic Ocean, NW Iberian Peninsula) is a flat-topped seamount located about 200 km from the northwest coast of Spain. This bank is included in the LIFE+ “INDEMARES” project, who aims to identify priority areas of conservation in the Spanish seas. In 2010 and 2011 two oceanographic surveys were carried out to investigate species and habitats of this deep ecosystem. A total of 28 stations were sampled using a box corer with a sampling area of 0.09 m2, in order to evaluate the distribution and biodiversity of the macroinfauna of the Galicia Bank. An additional sediment sample was taken at each station to analyse the granulometric composition and the organic matter content. Sediments were mainly sandy in nature (medium, fine and very fine sands), with low levels of organic matter content. The samples analysed yielded a total of 1189 individuals, belonging to 89 families. Polychaetes were the best represented group in total number of individuals (67%), followed by molluscs (14%). Echinoderms (9.7%), crustaceans (6%), and the Others group (Nemertea and Sipuncula) (3.9%) were less abundant. Two major macrobenthic assemblages were determined through multivariate analyses. Sedimentary composition was the main factor structuring the benthic community, separating medium sand stations from those that had finer sediments

Workshop on adult egg production methods parameters estimation in mackerel and horse mackerel (WKAEPM). ICES scientific reports.

The Workshop on Adult Egg Production Methods Parameters estimation in Mackerel and Horse Mackerel (WKAEPM) looked at the imprecision between institutes when processing survey samples. A number of protocol improvements were proposed, and these will be in place prior to the adult parameter analysis in 2022. A calibration exercise was carried out prior to the workshop using standard mackerel and horse mackerel egg survey (MEGS) protocols. A second exercise was conducted during the workshop using a newly developed SmartDots module. Subgroups dealt with issues regarding annual egg production method (AEPM) and daily egg production method (DEPM) and added their recommendations to the manuals. Descriptions for spent and massive atresia terms used during the screening process were redefined by adding further text and higher quality images into the ICES Survey Protocol Manual for the AEPM and DEPM estimation of fecundity in mackerel and horse mackerel (SISP- 5). Differences were noted in post ovulatory follicle (POF) and early alpha atresia identification, showing the difficulty associated with this work. In fecundity samples, there was high variance when identifying small oocytes close to the 185µm size threshold. It was recommended to have all fecundity samples analysed by two readers, and new criteria for the measurement of small oocytes were agreed. In atresia analysis, high variance was observed in both point and profile counting. High-resolution images are essential for this work, thus in 2022 slide scanner pictures will be taken for atresia analysis and will be sent around to all labs. There is still poor consensus on POF staging. Misclassifications between recent POFs and artefacts have now been clarified. Recent POF stages are used in spawning fraction estimation thus it is vital to be clear about them. A reference catalogue of images of early alpha atresia and POFs will be compiled and stored in SmartDots. The desired number of gonad samples to be collected during the egg surveys, including North Sea samples, was defined. WGMEGS has requested that additional mackerel and horse mackerel female gonad samples would be collected by the Blue whiting survey, the Irish WESPAS survey and the Dutch Pelagic Fisherman’s Association, PFA. An updated version of the ICES Fecundity and Atresia database will be ready for testing at the beginning of 2022 and the survey protocol manual will be updated in 2024

Estimación área de la Unidad Funcional de Cigala 25 (Galicia Norte) para el diseño de la campaña ISUNEP25_062022

ISUNEP2