In 1979 the Marine and Limnology Research Center (CIMAR) was established at the University of Costa Rica. Since then more than 1 000 scientific papers have been published by local and visiting scientists, a milestone that is the main motivation for this special issue of the Revista de Biología Tropical. The study of intertidal and shallow water ecosystems of both Pacific and Caribbean coasts was and continues to be a priority.

Most of the early CIMAR research on the Pacific coast focused on the Gulf of Nicoya estuary, an important fishing ground and the site of the main Pacific port facilities of Costa Rica. Nearly 100 papers on the biology, physics and chemistry of the waters and sediments of the estuary were released during the 1980s, mainly as part of an international collaborative effort that allowed the 15 m long RV Skimmer (University of Delaware, USA) to operate in the Gulf (Vargas, 1995). The diversity of epibenthic and infaunal invertebrates from the Gulf was evaluated by sampling with grab, and trawl, respectively, to a depth of 65 m. (Maurer & Vargas, 1984; Maurer et al., 1984). The first report on trace metals in invertebrates and sediments from the Gulf was published by Dean, Maurer, Vargas, & Tinsman (1986). The study of tidal flats in the Gulf of Nicoya followed as a key area of research (Vargas, 1996; Ditmann & Vargas, 2001).

In the 1990’s international cooperation made possible joint cruises aboard the 50 m long RV Victor Hensen (Zentrum fur Marine Tropenokologie, Bremen, Germany), which allowed deeper sampling in other Pacific coastal embayments. Box corer and trawl nets were used to study the fauna and biogeochemistry of sediments to depths of 200 m in the Gulf of Nicoya, the Golfo Dulce anoxic basin, and Coronado Bay (Wolff, Chavarría, Koch, & Vargas, 1998; Dalsgaard, Canfield, Peterson, Thamdrup, & Acuña-González, 2003).

More recently, collaboration with private deep-sea shrimp trawling vessels has facilitated the study of benthic fauna at depths near 350 m along the Pacific coast of Costa Rica (Wehrtmann, Herrera-Correal, Vargas, & Hernáez, 2010). Another cooperative effort allowed access to the Deep See submersible (Undersea Hunter Group) to study the deep water (450 m) at the Isla del Coco National Park, a Pacific site located 300 nautical miles from the Gulf of Nicoya (Cortés & Blum, 2008; Starr, Cortés, Barnes, Green, & Breedy, 2012).

Joint biological research in waters deeper than 400 m has been sporadic. Deep water surveys on the Pacific coast of Costa Rica have emphasized the geochemisty and biology of cold seeps and similar environments, particularly the Jaco Scar, South of the Gulf of Nicoya, and Mounds 11 and 12 West of Coronado Bay (Levin et al., 2012). According to Levin (2005) cold seeps occur in the sea floor where reduced sulphur and methane reach the surface without an important rise in water temperature. The macrofauna of cold seeps of Costa Rica includes tubeworms, clams, mussels, and microbial mats (Suess, 2014).

Several new species of deep sea invertebrates have been described by visiting scientists based on material collected in Costa Rica, including deep sea clams such as those found by Barry & Kochevar (1999) and Martin & Gofredi (2012). The finding in 2009 at a depth of 1 000 m on Mound 12 and follow up description by visiting and local scientists of a new species of antiphatatian coral (Opresko & Breedy, 2010) is a notable exception.

In 2005 a geochemistry cruise aboard the RV Atlantis (AT-11) using the Deep Sea Research Vessel (DSRV) Alvin (Dive 4129) focused on the Jaco Scar (Furi et al., 2010). According to Mau, Rehder, Sahling, Schleicher, & Linke (2012), the Jaco Scar, which extends from 1 000 m to 2 400 m deep, is a slide of the ocean floor caused by seamount subduction. There methane rich fluids lead to the hydrogen sulfide used by most vent fauna as an energy source.

Samples of coastal bivalve mollusks from the Gulf of Nicoya were being analyzed at the time for metal concentrations (Vargas, Acuña-González, Gómez, & Molina, 2015) Most of the reports on trace metals in deep sea clams come from specimens collected at hydrothermal vents, where strong water temperature gradients are typical. Thus, the access to samples of bivalves from the Jaco Scar cold seep was kindly allowed upon request by the senior author. Tissue samples from these mollusks were included in the metal analysis and the results reported herein.

The objective of this study is to report data on trace metals in tissues of vesicomyid clams, and in a mussel, sediment, and rock samples from the Jaco Scar, and to provide morphometric data of the clam shells.

MATERIALS AND METHODS

Mollusks were collected on June 13th, 2005 during dive 4129 of the DSRV Alvin operated from RV Atlantis (Cruise AT-11) at Jaco Scar (09-06.836 N - 84-50.408 W) at a depth of 1 888 m. The site is located south of the mouth of the Gulf of Nicoya estuary and is inhabited by chemosynthetic communities that include bacterial mats, vesicomyid clams, mussels, tube worms, and other invertebrates (Furi et al., 2010).

After collection, the bivalves were frozen on board the ship and later transported to the CIMAR laboratory in a plastic cooler. The collection included one specimen of deep-sea mussel and 13 specimens of vesicomyid clams (Numbered 01 to 13) of which five were preserved whole (shells and tissues) in 90 % ethyl alcohol. A rock fragment was also collected. A small clam (# 08) was found dead at the time of collection and had the space between valves filled with soft dark gray sediment. Seven clams were open and soft parts removed with a plastic knife and stored frozen (-18 oC) until analyses. A valve (usually the right one) of each of the seven clams was weighed (grams) for reference. The 13 clams were measured to the nearest mm for length (L), height (H), and width (W, both valves attached, when intact) and ratios (H/L, W/L, W/H) computed. Distance from the umbo to the anterior region was also measured. Empty shells and whole specimens were deposited in the mollusk collection of the Museum of Zoology, University of Costa Rica (MZUCR).

Nine metals (Aluminum, Cadmium, Copper, Iron, Lead, Manganese, Nickel, Tin and Zinc) were selected for analysis. All metal determinations were performed as described in Vargas et al. (2015): Tissue samples were weighed after drying in an oven at 65 ºC for 48 h. The rock fragment from the site, as well as the sediment trapped in clam #08, were included in the metal analysis. Dried samples were ground to powder and sub-samples of 1.00 g to 4.00 g placed in Teflon containers with 6 mL of high purity nitric acid, 2 mL of high purity hydrochloric acid, and pressure-digested in a microwave oven (CEM® MARSx). After digestion, the containers were left to reach room temperature, the liquid was transferred to 100 mL volumetric flasks, and diluted with deionized water. Certified reference materials and blank tests were also run. Cu, Fe, Mn and Zn were analyzed by Flame Atomic Absorption Spectrometry (Perkin Elmer® 3300) and Al, Cd, Ni, Pb and Sn by Graphite Furnace Atomic Absorption Spectrometry (Perkin Elmer® HGA 600). Calibration curves were produced against certified standards for each element according to the UCR-CICA accredited protocols. Concentrations were determined in triplicate. The results are expressed in μg/g dry weight (dw). Detection limits typical values (μg/g) were: 18 for Zn, 1.9 for Fe, 0.40 for Al, 0.10 for Sn, 0.027 for Pb, 0.022 for Ni, and 0.0020 for Cd. Detection limitis for Cu and Mn were 6.7 ug/g and 2.2 ug/g, respectively.

RESULTS

A total of 13 vesicomyid clams and one mussel were collected (Table 1, Figs. 1 and 2). External and internal views of the valves of one of the larger clams (#04) collected are included in Fig. 1 A, B, respectively. A hand drawing of the external and internal view of another clam (#07) is illustrated in Fig. 1 D, E. Details of hinges of clams 04 and 07 are included in Fig. 1C, F, G, respectively. Recently collected clams had a sulfur odor and tissues and shells were smeared with a red pigment (Fig. 1H, I). Photographs of the 13 clams are included in Fig. 2, as and aid for future identification of the species name. The surface of the clams had a chalky appearance and a deshicent olive brown periostracum was present mostly near the edges (Fig. 2). Morphometric data as well as the ratios of H / L, W / L, and W / H are listed in Table 1. The shortest and longest valves measured 87 mm and 200 mm, respectively. H / L valve ratios ranged from 0.37 to 0.43. The right valve of the longest shell weighed 76 grams and had a thickness of about 2 mm at its center (Table 1). The catalogue codes for the malacology collection of the Museum of Zoology, University of Costa Rica (MZUCR) for each of the eight shells and five whole specimens of clams are also listed in Table 1. The only mussel collected had a length of 130 mm (Fig. 1J), and had a thin and brittle shell.

Concentrations of nine metals (Aluminum, Cadmium, Copper, Iron, Lead, Manganese, Nickel, Tin and Zinc) in tissue samples from seven clams, the mussel, sediment, and the rock from the site are inclued in Table 2. The concentrations (µg/g), in decreasing order and range, in clam tissues were: Zn (43.3 - 266.3) > Fe (27.2 - 100.0) > Al (5.08 - 69.9) > Cd (0.11 - 12.23) > Sn (2.85 - 9.50) > Cu (4.0 - 7.3) > Mn (1.1 - 2.2) > Pb (0.24 - 0.79) > Ni (0.188 - 0.582). The gills had the maximum concentrations of Fe and Al. Higher concentrations of Pb, Zn and Sn were found in muscle tissues, while Cd, Cu, Mn an Ni were found in higher concentrations in foot tissues.

Maximum concentrations (µg/g) of metals in tissues of the only specimen of mussel collected, were: Zn (80.4 - gills), Fe (70.6 - gills), Al (26.6 - gills), Sn (4.87 - mantle), Cu (31.0 - gills), Mn (1.7 - mantle), Ni (0.97 - muscle), Pb (0.699 - muscle), Cd (0.575 - gills). Concentrations (µg/g) of metals in the sediment trapped in shell #10, were: Al (40 800), Fe (26 500), Mn (72.0), Zn (64.7), Cu (29.4), Ni (19.3), Sn (15.56), Pb (2.98), Cd (0.16). Metals (µg/g) in the rock fragment were: Fe (15 650), Al (9 240), Mn (169.9), Sn (99.5), Zn (36.5), Ni (20.4), Cu (13.4), Pb (1.63), Cd (traces).

A comparison of metal concentrations (µg/g) found in this study, with four reports from the literature is included in Table 3, together with data on metals in the razor clam Tagelus affinis from a sand flat in the Gulf of Nicoya.

DISCUSSION

Hydrothermal vents and cold seeps are deep-sea environments discovered during the last decades of the twentieth century, thanks in part to the development of human-occupied vehicles (HOVs), remotedly operated vehicles (ROVs) and high-resolution sea floor mapping. Seeps are benthic systems supported by both soft sediments and carbonate rocks. Clams of the family Vesicomyidae usually form large clusters in the sediments and mudstones of these sites (Levin et al., 2015). Originally considerd as different systems, recent evidence points to the existence of intermediate hydrothermal-seep environments along a continuum (Levin et al., 2012).

Aggregations of deep sea clams generally include more than one species at a site, the species composition varying with environmental conditions, and the presence of cryptic species complexes is expected (Watanabe et al., 2013). Plasticity in shell morphologies is also a problem for the identification of species. The subfamily Plioclardiinae includes relatively large clams living in a depth range of 100 to 6 809 m. The majority of the nearly 110 species are associated to cold water hydrocarbon seeps (Johnson, Krylova, Audzijonyte, Sahling & Vrijenhoek, 2017).

On the Pacific coast of Costa Rica, the seep sites known as Mound 11, Mound 12 and Jaco Scar are characterized by chemosynthethic macrofauna (clams, mussels, tube worms), authigenic carbonate rocks, and fine sediments (Furi et al., 2010). The Jaco Scar is an example of a site that has organisms with affinities to both vents and seeps. Its biodiversity appears relatively higher in comparison with other vents and seeps, since the presence of many yet undescribed species of mollusks is noteworthy (Levin et al., 2012).

The number on published papers on deep-sea environments from the Pacific coast of Costa Rica is on the rise. Most of these studies have collected vesycomyid clams and the specimens have been assigned to different species names:

Vesicomyid clams, found partially buried in sediments at cold seeps sites located between 2 900-3 800 m near the Jaco Scar, were described as C. diagonalis by Barry & Kochevar (1999). They provide shell measurements and ratios to separate C. diagonalis from six other vesicomyid clam species. Their paratype collected in Costa Rica measures 201 mm and has a H/L ratio of 0.39 The largest clam found during Alvin dive 4129 is 200 mm long and has a H/L ratio of 0.40 However, the W/L ratio (0.26) of C. diagonalis Costa Rican paratype is less than those (mean = 0.30) of clams from dive 4129. Clam #08 from dive 4129 has a dentition similar to C. diagonalis.

The study by Peek, Gaut, Feldman, Barry, Kochevar, Lutz, & Vrijenhoek (2000) is among the earlier reports on vesicomyids associated to cold seeps on the Pacific coast (09o N - 86o W) of Costa Rica. The clams, collected at depths of 3 000 m in soft sediments, were designated as Ectenagena extenta, Calytogena pacifica, and as “large- bodied” unidentified.

The review by Krylova & Sahling (2006) includes 12 genera of Vesicomyid clams of which only two (Phreagena and Pleurophopsis) were listed as having shell lenghts near 200 mm. More recently Krylova & Sahling (2010) indicates that an undescribed species of Archivesica and the genera Laubiericoncha and Phreagena are present off Costa Rica.

A study of water chemistry at the Jaco Scar and the use of ROV video footage of the benthic fauna by Mau et al. (2012) pointed out to the existence of dense patches of vesicomyid clams identified as Calyptogena spp.

Levin et al. (2012) studied the bottom fauna of the Jaco Scar (9o7.05’ N - 85o50.39’ W) at depths from 1 752 m to 1 805 m. They found that the macrofauna was characterized by clams identified as Archivesica gigas. The mussels included new taxa close to Bathymodiolus thermophilus.

In another survey of the Jaco Scar, the new versicomyid ‘Pliocardia’ krylovata, was described based on 15 specimens collected in 2009 at a depth of 740 m at the Jaco Scar summit an at near 1 000 m depth at Mound 12 (Martin & Gofredi, 2012). However, P. krylovata is relatively small and subovate in shape (length 31 to 59 mm, H / L ratio 0.70 to 0.90) when compared with the 13 specimens from dive 4129.

Coan &Valentich-Scott (2012) focused on the bivalves of tropical West America and provide photographs of the right valves and dentition of 15 species of vesicomyid clams, including A. gigas, C. costarricana, C. diagonalis, C. magnifica, L. angulata, and Phreagena kilmeri. The photographs (p.528) by Coan &Valentich-Scott (2012) that share most resemblance with those from dive 4129 correspond to P. kilmeri. However, the ratio H/L for P. kilmeri listed by Barry & Kochevar (1999) is 0.51, which is higher than the maximum (0.43) measured in this study.

Audzijonyte, Krylova, Sahling, & Vrijenhoek (2012) report the presence on the Costa Rican Pacific Accretionary Wedge of undescribed species of vesicomyid clams of which several were provisionally assigned to the genus Archivesica.

Based on the above mentioned reports and morphological data, the clams found during dive 4129 at the Jaco Scar probably belong to the genus Archivesica. Further taxonomic work is needed to confirm this possibility.

Metal concentrations in low temperature fluids, such as those present in cold seeps, are expected to be lower than those in high temperature hydrothermal vent fluids (Koshinsky, Kaush, & Borowski, 2014) Several groups of the nearby benthic macrofauna bioaccumulate many metals (Demina, 2016) However, most of the data on trace metals in tisses of deep sea mollusks comes from specimens collected at hydrothermal vents.

The pioneer study by Roesijadi & Crecelius (1984) on trace metals in vesicomyid clams provides data for C. magnifica from a hydrothermal vent on the East Pacific Rise (21o N - 109o W) at a depth of 2 600 m. Highest concentrations (µg/g) of Fe and Cd were found in the gills, while the kidneys concentrated Pb, Cu, and Sn.

Ruelas-Inzunza, Soto, & Páez-Osuna (2003) studied metals in the clam Vesicomya gigas from a hydrothermal vent in the Gulf of California (27o N - 111o W). They found in the gills higher concentrations of Fe, Cd, Mn and Zn. Aluminum, Tin, and Nickel were not included. However, their order of decreasing concentrations (Zn > Fe > Cd > Cu > Mn > Pb) is the same as that found in our study for those metals.

Demina, Galkin & Shumilin (2009) studied the metals in one specimen of A. gigas from the same vent site in the Gulf of California. The decreasing order and range (Min / Max) of concentrations (µg/g) found, was: Zn (120 / 3110), Fe (125 / 452), Cu (9.2 / 45.5), Mn (8.6 / 11.5), Cd (1.12 / 4.32), and Pb (1.42 / 4.1) Zinc concentration in the gills had the highest concentration and widest range of any metal.

In clams of the Jaco Scar collected during dive 4129 the highest concentration (µg/g) of Fe (100) and Al (69.9) were found in the gills. The fact that gills accumulate more metals than other tissues in deep sea clams is a well known fact (Childress & Fisher, 1992).

In spite of the fact that most of the information on metals in clams come from hydrothermal vents rather than from seep sites, the following results from the Jaco Scar seep are noteworthy when compared with the above mentioned three reports: First, clam gills also appear to concentrate certain metals like Fe and Al. Second, concentrations of Fe were below the range reported for hydrothermal vents. Third, concentrations of other metals were generally near the lower range reported for hydrothermal vent sites.

Vesicomyid clams from vents are known to accumulate metals in concentrations higher than those found in certain bivalves from polluted shallower environments such as industrialized estuaries (Childress & Fisher, 1992). The Jaco Scar is located south of the mouth of the Gulf of Nicoya estuary. As a comparison of maximum concentrations (µg/g) of metals in non-depurted specimens of the intertidal razor clam, Tagelus affinis from a sand flat in the upper Gulf (Vargas et al., 2015) indicates that the razor clam accumulated certain metals more than the Jaco Scar clams, while other metals were within the range. However, T. affinis was able to lower concentrations of certain metals after a 72 h depuration in clean sea water (Vargas et al., 2015). Higher concentrations of Fe and Zn in tissues of T. affinis and other invertebrates from the sand flat were related to the presence of metal rich sediments at the site. Other metals were found in concentrations commonly found in non-industrialized estuaries (Vargas, Acuña-González, Vásquez, & Sibaja-Cordero, 2016).

In a study of several mid Atlantic hydrothermal vent fields, Koshinsky, Kaush, & Borowski (2014) reported concentrations of metals in the mussel Bathymodiolus spp. The maximum concentrations (µg/g) were: Fe (1 495), Cu (352), Zn (187), Pb (29.7), Mn (15.2), Cd (11.1). Higher concentrations of Cu, Zn, and Pb were found in the gills.

Concentrations of certain metals such as Fe, Cd, Mn and Pb from the Jaco Scar seep mussel were lower than those reported in mussels from the hydrothermal vent site, while Cu and Zn were within the range.

The Jaco Scar and Mounds 11 and 12 are promising ecosystems for future joint collaborative efforts involving multidisciplinary approaches.

ACKNOWLEDGMENTS

We thank K.M. Brown, for the collection of samples at the Jaco Scar during DSRV Alvin dive 4129. The metal analysis was made possible by grants from the Costa Rica-United States of America Foundation for Cooperation (CRUSA), and the University of Costa Rica (UCR). Projects 808-AO-506 and 808-A3-526. We thank Jenaro Acuña-González, Eddy Gómez and Jairo Garcia for their help in the chemical laboratory. The hand drawing of the shells was prepared by Fiorella Jiménez.

RESUMEN

Metales en los bivalvos del emisor frío de Jaco Scar, Costa del Pacífico de Costa Rica. La investigación del mar profundo ha hecho descubrimientos significativos gracias a la disponibilidad de mapeo batimétrico de alta resolución y vehículos capaces de llegar a emisores hidrotermales y emisores fríos. El margen continental del Pacifico de Costa Rica incluye emisores de metano habitados por almejas vesicómidas en las que es esperable la acumulación de metales. Son escasos los datos sobre metales en almejas de emisores fríos. Por lo tanto, los objetivos de este estudio son el presentar datos de las concentraciones de Al, Cd, Cu, Fe, Pb, Mn, Ni, Sb y Zn en muestras de siete almejas, un mejillón, sedimento y roca, junto con datos morfométricos. Los bivalvos (Archivesica sp.?) fueron recolectados en el 2005 a una profundidad de 1 888 m en el Jacó Scar (09o06’ N - 84o50’ W) durante la inmersión 4219 del DSRV Alvin. Los metales fueron analizados por Absorción Atómica de llama (FAAS) y Absorción Atómica en Horno de Grafito (GFAAS). Las concentraciones están en µg/g peso seco. El orden decreciente de concentraciones máximas y su ámbito en tejidos de siete almejas, fueron: Zn (43.4 - 266.3) > Fe (27.2 - 100.0) > Al (5.0 - 69.9) > Cd (0.11 - 12.23) > Sn (2.8 - 9.5) > Cu (4.0 - 7.3) > Mn (1.1 - 2.2) > Pb (0.24 - 0.79) > Ni (0.19 - 0.58). Las branquias tenían las máximas concentraciones de Fe y Al. Las concentraciones máximas en el único ejemplar de mejillón, fueron: Zn (80.4 – branquias), Fe (70.6 - branquias), Cu (31.0 - branquias), Al (26.6 - branquias), Sn (4.87 - manto), Mn (1.7 - manto), Ni (0.97 - músculo), Pb (0.69 - músculo), Cd (0.57 - branquias). La muestra de sedimento contenía: Al (40 800), Fe (26 500), Mn (72.0), Zn (64.7), Cu (29.4), Ni (19.3), Sn (15.5), Pb (2.98), Cd (0.16); mientras que el fragmento de roca contenía: Fe (15 650), Al (9 240), Mn (169.9), Sn (99.5), Zn (36.5), Ni (20.4), Cu (13.4), Pb (1.6), Cd (trazas). Las branquias de las almejas concentraron metales come el Fe y el Al. El Fe estuvo bajo el ámbito reportado para almejas de emisores hidrotermales, mientras que las concentraciones de otros metales estuvieron cerca del ámbito inferior. Las concentraciones de Fe, Cd, Mn, y Pb en tejidos del mejillón fueron menores que las de mejillones en emisores hidrotermales, mientras que las de Cu y Zn estuvieron dentro del ámbito. Metales en las muestras de sedimento y roca son muy ricas en ciertos metales como Al y Fe y muy pobres en otros, como el Cd. Existe una escasez de datos sobre metales y contaminantes en almejas y otras especies de la macrofauna en emisores fríos de Costa Rica. Los datos presentados deben ser complementados en estudios futuros sobre la geoquímica, biología y manejo de estos sistemas.

Palabras clave: emisores de metano, Vesicomyidae, Plioclardiinae, tectónica, subducción.

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Table 1

Morphometric data in mm (Length, Heigth, Width, ratios H/L, W/L, W/H) and length Umbo to Anterior margin

(U to AM) of the vesicomyid clams. Jaco Scar, Pacific coast of Cosfa Rica (9º 06’ N - 84º 50’ W).

DSRV Alvin dive 4129, June 13th, 2005

Specimen	Length	Height	Width	H / L	W / L	W / H	U to AM	Weight (g)
Shells
MZUCR10425-01	160	64	44	0.40	0.28	0.68	47	44
MZUCR10425-02	150	59	46	0.39	0.31	0.78	38	33
MZUCR10425-03	162	62	**	0.38	**	**	40	51
MZUCR10425-04	188	71	59	0.38	0.31	0.83	48	58
MZUCR10425-05	175	68	55	0.39	0.31	0.83	45	56
MZUCR10425-06	200	80	**	0.40	**	**	50	76
MZUCR10425-07	163	67	60	0.41	0.37	0.89	45	54
MZUCR10425-08	87	38	31	0.43	0.39	0.81	37	7
Whole
MZUCR10425-09	170	63	49	0.37	0.29	0.78	35
MZUCR10425-10	160	64	51	0.40	0.32	0.79	35
MZUCR10425-11	170	69	58	0.40	0.34	0.84	43
MZUCR10425-12	133	57	47	0.43	0.35	0.82	34
MZUCR10425-13	175	67	63	0.38	0.36	0.94	40

Table 2

Concentrations (µg/g) of metals (Fe, Cd, Pb, Zn, Cu, Mn, Ni, Sn, Al) in tisúes (foot, muscle, gill, mantle), and mean

(n = 3) determined by FAAS and GFAAS in specimens of clams (Vesicomyidae), a mussel, sediment and rock from

1 888 m depth, Jaco Scar, Pacific coast of Costa Rica (9º 06’ N - 84º 50’ W). DSRV Alvin dive 4129, June 13th, 2005

Tissue	Fe	Cd	Pb	Zn	Cu*	Mn*	Ni	Sn	Al
Clams
Foot 01	68.4 + 4.1	12.23 ± 0.85	0.43 ± 0.14	264.3 ± 4.4	<3.7	<1.1	0.331 ± 0.079	6.83 ± 0.12	13.81 ± 0.34
Foot 03	27.2 ± 4.4	0.286 ± 0.025	0.24 ± 0.17	72.56 ± 0.93	<4.2	<1.3	<0.22	5.26 ± 0.18	19.33 ± 0.47
Foot 05	80.3 ± 3.5	0.612 ± 0.055	0.751 ± 0.065	261.3 ± 9.3	<7.3	<2.2	0.582 ± 0.066	2.85 ± 0.19	24.60 ± 1.50
Foot 07	57.2 ± 2.0	0.165 ± 0.019	0.722 ± 0.037	166.5 ± 5.3	<4.0	<1.2	0.396 ± 0.036	3.54 + 0.16	13.50 ± 1.50
Muscle 02	41.6 ± 4.4	0.330 ± 0.043	0.35 ± 0.16	74.19 ± 0.91	<4.1	<1.3	0.188 ± 0.092	5.87 ± 0.18	10.53 ± 0.25
Muscle 04	38.8 ± 3.7	0.399 ± 0.029	0.51 ± 0.13	43.37 ± 0.48	<3.5	<1.1	0.512 ± 0.074	9.50 ± 0.18	5.08 ± 0.12
Muscle 05	81.8 ± 2.9	0.192 ± 0.027	0.787 ± 0.053	266.3 ± 8.1	<6.0	<1.8	0.569 ± 0.054	6.44 ± 0.28	10.91 ± 0.91
Muscle 06	55.5 ± 2.9	0.110 ± 0.026	0.544 ± 0.053	88.4 ± 2.2	<6.0	<1.8	0.311 ± 0.057	3.14 ± 0.17	7.64 ± 0.63
Gills 03	100.0 ± 3.3	0.131 ± 0.029	0.375 ± 0.061	117.4 ± 4.1	<6.7	<2.0	0.274 ± 0.064	2.94 ± 0.18	69.90 ± 4.50
Mantle 04	76.9 ± 2.9	0.526 ± 0.047	0.523 ± 0.054	72.9 ± 2.0	<6.1	<1.8	0.402 ± 0.056	4.17 ± 0.20	25.7 ± 1.50
Mussel
Muscle	29.8 ± 2.5	0.456 ± 0.041	0.699 ± 0.046	34.65 ± 0.75	<5.2	<1.6	0.972 ± 0.050	4.62 ± 0.21	11.63 ± 0.98
Mantle	20.6 ± 2.9	0.132 ± 0.026	0.516 ± 0.052	29.44 ± 0.74	<5.8	<1.7	0.778 ± 0.053	4.87 ± 0.22	9.30 ± 0.89
Gills	70.6 ± 2.1	0.575 ± 0.050	0.512 ± 0.035	80.4 ± 2.4	31.0 ± 2.2	<1.2	0.346 ± 0.035	3.05 ± 0.14	26.60 ± 1.70
Sediment	26 500 ± 1 200	0.158 ± 0.014	2.98 ± 0.18	64.7 ± 1.6	29.4 ± 2.0	72.0 ± 2.2	19.3 ± 1.1	15.56 ± 0.67	40 800 ± 3 000
Rock	15 650 ± 490	<0.0023	1.63 ± 0.15	36.48 ± 0.42	13.38 ± 0.75	169.9 ± 5.4	20.41 ± 0.48	99.5 ± 2.5	9 240 ± 210

The uncertainty (±) corresponds to the expanded uncertainty using a coverage factor k = 2.

* Detection limits vary between samples since LD depends upon linear regression for each metal, the complexity of the matrix as well as the sample amount digested.

Table 3

Concentrations (ug/g) of metals (Fe, Cd, Pb, Zn, Cu, Mn, Ni, Sn, Al) in tissues of: deep sea clams

reported in three previous studies (A,B,C), and in this study (D). Metals (ug/g) in: the mussel, Bathymodiolus

(E), the Jaco Scar mussel (F), the intertidal razor clam, Tagelus affinis (G)

Tissue	Fe	Cd	Pb	Zn	Cu	Mn	Ni	Sn	Al
Clams
A	760 ± 240	9.8 ± 0.8	6.0 ± 2.4	2152 ± 495	148 ± 10	5 ± 2	< 2.5	< 10.0	< 150
B. Mantle	277.5 ± 27	12.3 ± 5.5	3.67 ± 1.8	419.1 ± 79	29.7 ± 11.1	10.6 ± 1	ND	ND	ND
B. Gills	403.2 ± 242	115.2 ± 196	2.89 ± 2.5	844.8 ± 1 042	8.26 ± 5.8	18 ± 17	ND	ND	ND
C	125 to 452	1.12 to 4.32	1.42 to 4.1	120 to 3 110	9.2 to 45.5	8.6 to 11.5	ND	ND	ND
D	27.2 to 100.0	0.13 to 12.23	0.24 to 0.79	43.3 to 266.3	4.0 to 7.3	1.1 to 2.2	0.19 to 0.58	2.85 to 9.50	5.08 to 69.9
Mussel
E	196 to 1 495	1.3 to 11.1	1.2 to 29.7	65 to 187	23 to 352	3.2 to 15.2	ND	ND	ND
F	20.6 to 70.6	0.132 to 0.575	0.512 to 0.699	29.44 to 80.4	5.2 to 31	1.2 to 1.6	0.346 to 0.972	3.05 to 4.87	9.3 to 26.6
G. T. affinis	2160	0.69	1.37	206.7	21.6	255.2	4.13	3.74	ND

ND = No data. A. Roesijadi & Crecelius, (1984). B. Ruelas-Inzunza, Soto & Paez-Osuna, (2003). C. Demina, Galkin, & Shumilin, (2009). D. This study, clams, data from Table 2. E. Koshinsky, Kaush, & Borowski, (2014). F. This study, mussel, data from Table 2. G. Vargas, Acuña-González, Gómez, & Molina, (2015), maximum concentrations.