- Marine Record
- Open Access
Spiculosiphon oceana (foraminifera) and its affinity to intermediate stress conditions in the Panarea hydrothermal complex (Mediterranean Sea)
Marine Biodiversity Records volume 12, Article number: 23 (2019)
Spiculosiphon oceana Maldonado, López-Acosta, Sitjà, Aguilar, García & Vacelet, 2013 is a Mediterranean endemic giant stalked foraminifer described as a potential bio-indicator of acidic environments, thanks to its ability to cope with stressful chemical conditions. Here, we present the first record and the first video images of living specimens of this giant foraminifera in the Panarea Volcanic Complex (PVC; southern Tyrrhenian Sea), representing the third discovery worldwide. Specimens of S. oceana were identified through microscopic and remotely operated vehicle (ROV) image analyses, in two different areas characterised by water column physico-chemical parameters typical of the non-vented areas, but with some evidence of hydrothermal alteration. This new finding enhances knowledge on the ecology of S. oceana, enlarges its known spatial distribution, and corroborates its affinity to intermediate stress conditions related to hydrothermal activity.
Spiculosiphon oceana Maldonado et al. 2013 is a recently discovered endemic species of the Mediterranean Sea and is one of two species of the genus Spiculosiphon Christiansen 1964 recognised worldwide. These are large astrorhizids with a distinctive stalked test comprised of sponge spicules directly agglutinated in an organic wall (Maldonado et al. 2013; Di Bella et al. 2016, 2018). The type species, Spiculosiphon radiatus Christiansen 1964, was discovered in a Norway fjord at 100 m depth, while S. oceana was first described by Maldonado et al. (2013) at 153 m depth on a soft bottom on the “Seco de Palos” Seamount (western Mediterranean Sea, Spain). Probably another species of this genus, called Spiculosiphon cf. radiata, was recognised 18 years ago by Onno Gross in a dark sublittoral cave in the north-west Mediterranean Sea, but this record was never published (Maldonado et al. 2013).
The distinctive traits among the known species mainly concern the size: S. radiata is 2 cm long, while S. oceana is a giant foraminifer that can reach 3–4 cm in length (Maldonado et al. 2013). In addition, these foraminifera have a peculiar test standing on a hollow tube, that in S. oceana is characterised by a bulb-like proximal end, not observed in S. radiatus, that penetrates into the substratum but is never anchored permanently to it, and a globe-like capitate region (the distal end of the tube). Most of the test stands out of the marine bottom and is comprised of fragments of siliceous sponge spicules disposed along the major axis of the stalk. In the globe-like region, the spicules are arranged in a less agglutinated structure that allows the extrusion of the pseudopodia that, in turn, are sustained by a spherical crown built by radiating tracts of highly selected aciculate spicules. The resulting body morphology allows S. oceana to capture small planktonic demersal prey such as crustaceans or calcareous foraminifera (Maldonado et al. 2013).
A recent study reported the occurrence of S. oceana on the Zannone Hydrothermal Field (central Tyrrhenian Sea), highlighting its ability to cope with chemical conditions related to hydrothermal fluid emissions (Di Bella et al. 2016). This finding led to the speculation that S. oceana could be considered as a proxy of acidic environments (Di Bella et al. 2018).
Here, we present another record of S. oceana in the Mediterranean Sea, in the PVC (southern Tyrrhenian Sea). This new finding can enhance our knowledge of the distribution and habitat of S. oceana, and confirm its affinity to intermediate stress condition and its importance as a bio-indicator of recent ocean acidification processes related to hydrothermal activity.
Material and methods
Spiculosiphon oceana was discovered in November 2013, during the research cruise PANA13_04 conducted onboard the RV Astrea of ISPRA to explore the Panarea hydrothermal area, in particular the eastern slope of the north-northeast trending extension, north of Basiluzzo Islet (Fig. 1).
In this area, the hydrothermal activity is linked to radial volcano-tectonic processes that affect the slope, as evidenced by the presence of small-scale gullies radiating from the edge (Fig. 2a; Savelli et al. 1999; Romagnoli et al. 2013). Fe-rich deposits are widely distributed on the shelf edge (80–90 m), where they form crusts of iron-oxyhydroxides covered by silt deposits. While, on the steep slope (140–210 m) they give rise to numerous small chimneys of soft mud (black and red crusts with yellowish-orange precipitates on top), containing abundant semi-consolidated crusts of Fe-Mn oxyhydroxides (Gamberi et al. 1997, 1998; Savelli et al. 1999; Bortoluzzi et al. 2014).
Benthic communities were investigated by means of an ROV Pollux II equipped with a Nikon D80 high-resolution camera and a Sony HDR-CX560V full HD video camera. Two parallel laser pointers providing a 10-cm scale to measure in situ seafloor structures and macrobenthic organisms, and a small basket net enabling the collection of samples were also provided. One specimen of S. oceana was collected and preserved in situ in 90% ethanol solution and then analysed under a stereomicroscope Zeiss discovery v.8 equipped with micro-camera Axio-Cam vs40 v4.8.20. Water column data of temperature, salinity and pH were also acquired by a CTD SBE 911. A Crison pH 25 sensor was also used onboard to acquire data from the collected samples.
The analysed specimen of Spiculosiphon oceana was identified and photographed during the microscopic analysis of smooth sediments a few centimeters-thick, consisting of an Fe-encrusted deposit collected by the ROV from the top of a hydrothermal diffusive pinnacle-like structure described by Bortoluzzi et al. (2017) as a diffusive ferruginous seep (DFS), named DFS2 (Fig. 2).
This 2 m-high DFS was located at 204 m depth on the steep eastern slope of the Panarea platform elongation (north of the Basiluzzo islet) and was the result of a continuous and focused Fe-oxyhydroxide seafloor deposition of hydrothermal origin. It was characterized by the lack of visible gas bubbling and fluid emission, and by a top covered by thick reddish-orange iron-rich deposits containing complex and stratified communities of mainly ammonium- and iron-oxidising chemoautotrophs belonging to Thaumarchaeota, Nitrospira, and Zetaproteobacteria (Bortoluzzi et al. 2017). The main water column parameters, recorded in the area, showed rather constant temperature values of 14.1–14.3 °C, from 120 to 210 m depth. At the same depths, the acquired salinity was about 38.4 PSU, and the pH data ranged from a value of 8.1 to 8 (Table 1). The pH sensor, used onboard to acquire data from the collected sample, measured pH = 5 inside DFS2 structure.
The analysed specimen of S. oceana was recognised by its peculiar body morphology. Observation under the stereomicroscope allowed the identification of a fragment of the stalked test bearing the typical capitate region, but lacking the bulb-like structure (Fig. 3).
The stalk appeared as a rod (> 1.5 cm length) built by broken, agglutinated needle-like spicules (including a few long-shafted triaenes; Fig. 4a) disposed according to the major axis of the test, but slightly twisting around it (Fig. 4b) and arranged as reported in the specimens described by Maldonado et al. (2013) and Di Bella et al. (2018). Some sand grains were observed attached externally to the stalk (Fig. 4c), while, some broken portions of the test showed the internal organic layer (Fig. 4d).
The capitate structure appeared as a tangle of broken fragments of irregularly-shaped spicules arranged in a globular nucleus from which solid tracts (~ 1.5 mm length), composed by afew monoaxial spicules, radially extended (Fig. 5b). The analysed specimen of S. oceana showed only one of the radiating tracts, the others were probably broken during sampling and laboratory manipulation.
However, a detailed analysis of the ROV images, conducted after the identification of S. oceana in the study area, revealed several living specimens (> 20) with the typical stalked test (> 3.5 cm length; maximum measured length = 4.2 cm) and the globelike structure with the whole set of radiating tracts. These specimens were found standing out in iron-rich soft bottoms surrounding non-effusive hydrothermal structures at 140 m depth on the steep Basiluzzo slope (Figs. 2a and 5a), where only few Scyphozoa polyps (Cnidaria) were identified (Fig. 6). At these depths, no fluid emissions were observed; the temperature and salinity profiles in the water column were typical of the non-vented areas, as by the pH values (Table 1). Vent areas, affected by low temperature acidic fluids emission (Table 1), were located at a distance of about 2.3 km from the areas where S. oceana were found, at 85 m depth in the southeastern sector of the Basiluzzo hydrothermal system (Fig. 7).
The morphology of the stalked agglutinated astrorhizid analysed under the stereomicroscope and observed in ROV images, corresponds to that of the species originally described by Maldonado et al. (2013). Indeed, as reported, it is a giant foraminifer (> 3.5 cm) standing on a hollow stalk, built with highly-selected, long and thin spicule fragments, with a capitate globe-like structure bearing 20–30 slender radiating tracts not spiny, plumose or subdivided (Fig. 5).
Our finding represents the first record of Spiculosiphon oceana in the Panarea Volcanic Complex, the third in the whole Mediterranean Sea and the second record in a shallow-water hydrothermal area (the first being the Zannone Hydrothermal Field; Di Bella et al. 2016, 2018).
Previous studies recorded specimens of S. oceana temporally anchored on sand and detritic bottoms at depths ranging from 116 to 153 m (Maldonado et al. 2013; Di Bella et al. 2016, 2018). The observations of S. oceana along the Basiluzzo slope in the PVC extend the bathymetric distribution of the species down to 204 m. Specimens of S. oceana were recorded in two different areas characterised by absence of active fluid emissions and water column physicochemical parameters typical of the non-vented areas, although the presence of numerous DFS and iron and sulfur deposits and the low pH measured inside DFS seemed to indicate a shallow depth level of hydrothermal alteration (Bortoluzzi et al. 2014, 2017).
The collection of a few centimeters-thick Fe-encrusted deposit on the top of a DFS (204 m water depth) allowed us to reveal the presence of S. oceana in the PVC, then ROV underwater observations at − 140 m led to the identification of at least 20 specimens (maximum measured length = 4.2 cm; Fig. 5a) that may be many more considering the individuals shown in the Fig. 6. The specimens were found with most of the tests standing out of an almost defaunate soft bottom surrounding non-effusive hydrothermal structures and characterised by evidence of authigenic Fe-rich precipitation and sulfur deposition, typically observed along the northeast continental platform and down to the slope of Basiluzzo Islet (Marani and Gamberi 1997; Gamberi et al., 1999; Savelli et al. 1999; Esposito et al. 2015). In the two sampling areas, and more in general around 140 m depth, the sulphur deposits became more frequent and were commonly associated with microbial mats, that, as suggested by Di Bella et al. (2018), could represent an important food source available for S. oceana in hydrothermal habitat. On the other hand, the giant foraminifer was not found in the identified vent site, located at a distance of about 2.3 km, and characterised by active emission of low temperature acidic fluids, with pH rapidly decreasing from 8 to 7 near the sea bottom (Table 1).
These findings agree with the ecological features described by Di Bella et al. (2018) for S. oceana in the Zannone Hydrothermal Field (western Pontine Islands) where this giant foraminifer was not recorded in areas with strong hydrothermal emissions and most of the observed specimens were recorded in areas up to a distance of about 2 km from fluid emissions. This distribution pattern confirms the link between S. oceana and intermediate stress conditions that the foraminifer can cope with thanks to its peculiar morphological characteristics, while it seems to not tolerate the extreme acidic conditions of active venting fields.
This new record of Spiculosiphon oceana helps to understand the ecology of the species and enlarge its known bathymetric distribution. The wide living population of the foraminifer, showed for the first time in the present work in an area with some evidences of hydrothermal alteration (DFS, authigenic iron and sulphur precipitation and microbial mats) corroborates its affinity to intermediate stress conditions related to hydrothermal activity, strengthening the hypothesis, expressed by Di Bella et al. (2018), that this giant foraminifer could be considered a bio-indicator of acidic environments.
Availability of data and materials
All data generated or analyzed during this study are included in this published article.
Above sea bottom
Diffusive Ferruginous Seep
Practical Salinity Unit
Panarea Volcanic Complex
Remotely Operated Vehicle
Bortoluzzi G, Spagnoli F, Aliani S, Romeo T, Canese S, Grassi M, Masetti G, Dialti L, Cocchi L, Muccini F, Lacono V, Yakimov M, La Spada G, Ligi M, Giordano P, Franchi F, Ferrante V, Borgognoni L, Tudino T, Guideri M, Ivaldi R, Pratellesi M, Marziani F, Niccolini F, Barbieri E, Capaccioni B and Andaloro F. New geological, geophysical and biological insights on the hydrothermal system of the Panarea Basiluzzo Volcanic complex (Aeolian Islands, Tyrrhenian Sea). Congresso SGI-SIMP. 2014; 10–12 settembre Milano.
Bortoluzzi G, Romeo T, La Cono V, La Spada G, Esposito V, Sabatino G, Di Bella M, Canese S, Scotti G, Bo M, Giuliano L, Jones D, Golyshin PN, Yakimov MM, Andaloro F. Ferrous iron- and ammonium- rich diffuse vents support habitat-specific communities in a shallow hydrothermal field off the Basiluzzo islet (Aeolian volcanic archipelago). Geobiology. 2017; https://doi.org/10.1111/gbi.12237.
Christiansen BO. Spiculosiphon radiata, a new foraminifera from northern Norway. Astarte. 1964;25:1–8.
Di Bella L, Ingrassia M, Frezza V, Chiocci FL, Martorelli E. The response of benthic meiofauna to hydrothermal emissions in the Pontine archipelago, Tyrrhenian Sea (Central Mediterranean Basin). J Mar Syst. 2016;164:53–66.
Di Bella L, Ingrassia M, Frezza V, Chiocci FL, Pecci R, Bedini R, Martorelli E. Spiculosiphon oceana (foraminifera) a new bio-indicator of acidic environments related to fluid emissions of the Zannone hydrothermal field (Central Tyrrhenian Sea). Mar Environ Res. 2018;136:89–98.
Esposito V, Giacobbe S, Cosentino A, Minerva CS, Romeo T, Canese S, Andaloro F. Distribution and ecology of the tube-dweller Ampelisca ledoyeri (Amphipoda: Ampeliscidae) associated with the hydrothermal field off Panarea Island (Tyrrhenian Sea, Mediterranean). Mar Biodivers. 2015;45(4):763–8.
Gamberi, F.; Marani, M.P.; Parr, J.M.; Binns, R.A. Sub-seafloor mineralisation at the Panarea shallow-water platform, Aeolian volcanic arc, Italy. In: CSIRO Exploration and Mining, North Ryde, editor/s. Mineral Deposits: Processes to Processing; 1999; (Balkema, Rotterdam/Brookfield, 1999): 1999. 499–502. http://hdl.handle.net/102.100.100/210538?index=1.
Gamberi F, Marani M, Savelli C. Tectonic, volcanic and hydrothermal features of a submarine portion of the Aeolian arc (Tyrrhenian Sea). Mar Geol .1997;140:167–181.
Gamberi F, Savelli C, Marani MP, Ligi M, Bortoluzzi G, Landuzzi V, Lupi A, Costa M. Contesto morfotettonico e depositi idrotermali di solfuri ed ossidi di ferro in una porzione sommersa dell'arco eoliano (in base ad indagini ad alta definizione). Boll Soc Geol Ital. 1998;117:55–71.
Maldonado M, López-Acosta M, Sitjà C, Aguilar R, García S, Vacelet J. A giant foraminifer that converges to the feeding strategy of carnivorous sponges: Spiculosiphon oceana sp. nov. (foraminifera, Astrorhizida). Zootaxa. 2013;3669:571–84.
Marani M, Gamberi F. Savelli C shallow-water polymetallic sulphide deposits in the Aeolian island arc. Geology. 1997;25(9):815–8.
Romagnoli C, Casalbore D, Bortoluzzi G, Bosman A, Chiocci FL, D’Oriano F, Gamberi F, Ligi M, Marani M. Bathy-morphological setting of the Aeolian Islands. Geol Soc Lond Mem. 2013;37(1):27–36.
Savelli C, Marani M, Gamberi F. Geochemistry of metalliferous, hydrothermal deposits in the Aeolian arc (Tyrrhenian Sea). J Volcanol Geotherm Res. 1999;88:305–23.
The authors wish to thank the Captain Massimo Colorito, the crew of R/V Astrea for their professional support in the field work and Patrizia Perzia for technical assistance.
This study was funded by D.R.A. Assessorato Territorio Ambiente Regione Siciliana-Asse 3 Linea di intervento 18.104.22.168 of POR FESR Sicilia 2007–2013 aimed to assess the marine biodiversity in Sicily with a task WP3.2 focused on hydrothermal systems.
Consent for publication
The authors declare that they have no competing interests.
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
About this article
Cite this article
Esposito, V., Canese, S., Scotti, G. et al. Spiculosiphon oceana (foraminifera) and its affinity to intermediate stress conditions in the Panarea hydrothermal complex (Mediterranean Sea). Mar Biodivers Rec 12, 23 (2019). https://doi.org/10.1186/s41200-019-0183-4
- Large astrorhizids
- Shallow hydrothermal system
- Ocean acidification
- Panarea Island
- Aeolian archipelago