First records of Geodia demosponges from the New England seamounts, an opportunity to test the use of DNA mini-barcodes on museum specimens
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We report the first records of the sponge genus Geodia (Demospongiae, Tetractinellida, Geodiidae) from the New England Seamounts and Muir Seamount, at lower bathyal depths. Nine specimens collected between 2000 and 2005 belong to two boreal species (Geodia macandrewii and Geodia barretti) and a temperate species (Geodia megastrella). These records extend the distributions of these deep-sea amphi-Atlantic species to the west. Most of these specimens were originally fixed in formalin, which substantially degraded the DNA. We nonetheless managed to sequence two cytochrome c oxidase subunit I (COI) mini-barcodes: the universal mini-barcode at the 5′ end of the Folmer barcode (130 bp) and a newly proposed mini-barcode at the 3′ end of the Folmer barcode (296 bp). These mini-barcodes unambiguously confirmed our identifications. As an additional test, we also successfully sequenced these two mini-barcodes from the holotype of G. barretti, collected in 1855. We conclude by advocating the use of mini-barcodes on formalin-fixed or old specimens with degraded DNA.
KeywordsPorifera Geodia Mini-barcodes DNA barcoding DNA degraded Museum specimens
The first visual observations of the NES were made by camera drops in 1962 (Pratt and Thompson 1962) and the deep submersible vehicle (DSV) Alvin, on Bear Seamount in 1968 [Alvin dives 286 and 287, photos in Pratt (1968)] and on six other seamounts in 1974 (Nashville, Gilliss, Rehoboth, Manning, Balanus, and Mytilus), up to depths of 3,054 m (Houghton et al. 1977; Heirtzler et al. 1977). At that time, it was already clear that the most abundant benthic organisms were sponges (Demospongiae and Hexactinellida), especially on outcrops (Houghton et al. 1977). However, the fauna of the NES remained largely ignored until a series of Census of Seamounts (CENSEAM) campaigns in 2000–2005, part of the Census of Marine Life, began to collect and identify the fish and some invertebrates (Moore et al. 2003b, 2004). These campaigns clearly confirmed with video analysis that suspension feeders dominate these seamounts; the most abundant phyla in the NES were by far Porifera (sponges) at 54%, followed by Cnidaria (mainly corals) at 23% (Cho 2008). These studies also supported the idea that these seamounts represented biodiversity hotspots, which needed protection from deep-sea fishing. Thirteen seamounts from the NES and Corner Rise Seamounts were made Vulnerable Marine Ecosystem (VME) areas closed to fishing since 1 January 2007 (until 31 December 2020) and managed by the Northwest Atlantic Fisheries Organization (NAFO, http://www.fao.org/fishery/vme/23646/en). Moreover, some of these seamounts (Bear, Physalia, Mytilus and Retriever) in the US EEZ (Fig. 1) are, since 15 September 2016, included in the first marine national monument in the Atlantic called the Northeast Canyons and Seamounts Marine National Monument, where fishing and mining is now prohibited (NOAA 2016).
The 2000–2005 campaigns led to the discovery of several new genera and new deep-sea octocoral species (Pante and Watling 2012; Watling and France 2011; Cairns 2007; Watling 2007; Simpson and Watling 2011) but regrettably, although some sponges were observed and collected during these cruises, they were never formally described. Therefore, the sponge fauna in the NES is unknown apart from four tentative identifications: Hexactinellida Farrea sp. and Rossellidae sp., the demosponges Geodia sp., and Cladorhizidae sp. (Moore et al. 2003b; Cho 2008). The closest formal sponge records (570–800 km away) are from the Challenger Expedition (1872–76), which dredged around the Bermuda islands some deep-sea temperate Tetractinellida demosponges—Geodia pachydermata Sollas, 1886 (st. 56: 1,966 m), Stelletta tenuispicula Sollas, 1886 (station unknown) and Leiodermatium pfeifferae Carter, 1873 (st. 33: 795 m; st. 56) (Sollas 1888)—as well as deep-sea Hexactinellida—one species from station 33 and eight from station 56 (Schulze 1887). Otherwise, some 800–1,000 km northeast of the NES are many sponge records off Newfoundland, notably from the Grand Banks and Flemish Cap, where sponge abundance and diversity is high (Cárdenas et al. 2013; Murillo et al. 2012; Plotkin et al. 2017a, b).
The main aim of this study was therefore to identify a collection of Geodia specimens collected during the CENSEAM campaigns. Thanks to the revision of North Atlantic Geodia (Cárdenas et al. 2013; Cárdenas and Rapp 2015; Cárdenas et al. 2010; Cárdenas et al. 2011), we have solid morphological and molecular knowledge to identify these specimens. Because of the degraded nature of the DNA in these specimens, this study was also an opportunity to test the use of mini-barcodes for sponge species identification.
Material and methods
Specimens were collected during several NOAA New England Seamount campaigns that took place between 2000 and 2005: R/V Delaware II cruise DE00–11 (2000), R/V Delaware II cruise DE02–06 (2002), R/V Atlantis cruise AT07–35 (2003), R/V Atlantis cruise AT08–01 (2003), R/V Ronald H. Brown cruise RB04–04 (2004) and R/V Atlantis cruise AT12–01 (2005). Details on the R/V Delaware II cruises (2000–02) can be found in Moore et al. (2003b, 2004). Details of the other NOAA expeditions (2003–05) are available from the NOAA Ocean Explorer website (http://oceanexplorer.noaa.gov/explorations/explorations.html). Specimens were collected with a Yankee 36 bottom trawl (2000–02), with the DSV Alvin (2003–05) or with the remote operated vehicle (ROV) Hercules in the lower bathyal at depths between 1,489 and 2,829 m depth.
Pictures of the specimens were made on deck. Most specimens were bulk fixed in formalin before being transferred to 70% ethanol for long-term storage at room temperature. YPM 27001 is the only specimen to have been frozen on board (−20 °C freezer) and later fixed in 70% ethanol at the Peabody Museum of Natural History (YPM), Yale University, New Haven, USA. When these samples were sent to Uppsala University to be studied, they were sent in Carosafe® (a formaldehyde-free holding solution), and then stored back in ethanol before morphological and molecular studies. Today, these specimens are stored at the YPM at room temperature.
DNA was extracted using the DNeasy® Blood and Tissue kit (Qiagen, Hilden, Germany) in accordance with the manufacturer’s instructions. Sponge pieces were taken from the choanosome and lysed for 2 h in ATL buffer (Qiagen) with proteinase K. Extracted DNA was diluted and stored in 50 μl or 100 μl AE buffer (Qiagen) at −4 °C. Polymerase chain reactions (PCRs) were made in 25 μl solutions using PuReTaqTM Ready-To-Go™ PCR beads (GE Healthcare, Little Chalfont, UK). We tried to sequence the barcoding COI Folmer fragment (659 bp) on a Touchgene Gradient thermocycler (Techne, Cambridge, UK), using primers LCO1490 and HCO2198 (Folmer et al. 1994), the PCR program: [5 min/94 °C; 37 cycles (15 s/94 °C, 15 s/46 °C, 15 s/72 °C); 7 min/72 °C] and negative/positive controls. Although, the LCO/HCO primer pair is known to work on Geodia species (Cárdenas et al. 2010, 2011), our attempts were unsuccessful for all specimens except for YPM 27001.
To assess the quality and quantity of the DNA extractions, we first ran 1 μl of the extracted DNA on a 1.5% agarose gel. As expected from specimens fixed in formalin (Zimmermann et al. 2008, and references within), we observed smearing indicating degraded DNA, with highest intensity in the range of 100–500 bp. This range of sequences has been shown to be semi-stable in museum specimens (Zimmermann et al. 2008). The least degraded DNA came from YPM 027001, which had been frozen on board before being fixed in 70% ethanol. Further analyses on the Agilent 2200 TapeStation (Agilent Technologies, Santa Clara, CA, USA) with the High Sensitivity D1000 ScreenTape (Agilent Technologies) confirmed that several samples had very low DNA concentrations (22.1 pg/μl and lower), and sometimes too low to be detected.
Hajibabaei et al. (2006) developed the idea of sequencing a mini-barcode for such cases of museum specimens with degraded DNA. It has been shown that one can still amplify smaller sequences from degraded DNA and for this purpose, Meusnier et al. (2008) designed primers Uni-minibarF1 (~LCO) and Uni-minibarR1 to amplify a universal mini-barcode for animals, which corresponds to the first 130 bp of the Folmer fragment. Mini-barcodes have never been used in sponges. From the large Tetractinellida COI dataset from Kelly and Cárdenas (2016) opened in the alignment freeware AliView v.1.18 (Larsson 2014), we designed the degenerated primer Tetract-minibarR1 (5′-RAARAYCATTATAAGRCCRTGRGC-3′) with the exact same position and length as Uni-minibarR1 but more specific to the Tetractinellida. We then used the primer pair LCO/Tetract-minibarR1 and 2 μl of DNA template to amplify a 179-bp sequence (130 bp without primers), using the same thermocycler and PCR program described above.
According to a sub-alignment of only Geodia Folmer sequences, the universal mini-barcode would not be variable enough to discriminate the different species belonging to the Depressiogeodia clade (G. barretti, G. hentscheli and G. megastrella) (Cárdenas et al. 2011), so we also targeted a longer mini-barcode at the 3′ end of the Folmer fragment, which showed interspecific variation in this clade. For this purpose, we designed the new primer DepressioCOI393F (5′-GCCTCTATCGAGCGTTCAGG-3′); position 393 stands for the primer position in the COI of Amphimedon queenslandica Hooper and van Soest, 2006. We then used the primer pair DepressioCOI393F/HCO to amplify a 342-bp sequence (296 bp without primers), using the same thermocycler and PCR program described above. This mini-barcode will be called Depressio-minibarcode henceforth.
To test the use of universal mini-barcode and the Depression-minibarcode on old museum material, we also extracted the DNA from the dry holotype of Geodia barretti (NHM 18126.96.36.1999) collected on 6 August 1855 on the Western coast of Norway by Robert McAndrew and Lucas Barrett (McAndrew 1856; Bowerbank 1872). It is unclear how this specimen was preserved but it seems it was dried after collection (Bowerbank 1872; p. 198). The DNA extract was diluted in only 15 μl AE buffer since we anticipated its low concentration. Its concentration was measured using the Qubit® dsDNA BR Assay Kit (Invitrogen, Waltham, MA, USA) with a quantification range of 2–1,000 ng: the spectrophotometer could not detect any DNA in our extract. We nonetheless ran PCRs following the same protocol described above.
All PCR products were purified using the ExoSAP-IT® kit (USB Europe, Staufen, Germany) and sent for sequencing (Macrogen Europe, Amsterdam, The Netherlands) using the same primers as in the PCRs. Sequences were assembled and blasted using Geneious® 8.1 (created by Biomatters, http://www.geneious.com). When we had two COI mini-barcodes from the same specimen, we merged these sequences into a single one using the ‘merge’ option in AliView. Merged sequences (130 + 296 = 426 characters) were submitted to Genbank (KX982850–KX982854).
After digesting a piece of sponge tissue in chlorine, and washing the remaining spicules successively with water, 50% ethanol and 100% ethanol, spicules mounts were made using Eukitt™ mounting medium (Sigma-Aldich, St Louis, MO, USA). Twenty-five spicules per spicule type were measured, unless otherwise stated using a light microscope and an eyepiece micrometer. Observations of the pores were made with a stereomicroscope.
The following abbreviations are used for institutions mentioned in the text: BNHM, The Natural History Museum, London, UK; MNHN, Muséum national d’Histoire naturelle, Paris, France; ZMA, Zoological Museum in Amsterdam, The Netherlands (collection now moved to Naturalis, Leiden); ZMBN, Bergen Museum, Bergen, Norway; ZMUC, The Zoological Museum, Copenhagen, Denmark.
Taxonomy and results
We identified a total of three species of Geodia, all new records for this area: G. macandrewii (Bear Seamount), G. barretti (Muir Seamount) and G. megastrella (Picket, Kelvin, Manning and Muir Seamounts). Their distributions are shown in Fig. 1. We succeeded in sequencing the two mini-barcodes for all three species, including the 161-year-old holotype of G. barretti. Morphological and molecular studies were concordant. Collecting information and identifications results are available in the PANGAEA data repository (doi: 10.1594/PANGAEA.867276).
Class DEMOSPONGIAE Sollas, 1885
Subclass HETEROSCLEROMORPHA Cárdenas et al., 2012
Order TETRACTINELLIDA Marshall, 1876
Suborder ASTROPHORINA Sollas, 1887
Family GEODIIDAE Gray, 1867
Genus Geodia Lamarck, 1815
Geodia macandrewii Bowerbank, 1858
YPM 28261, Bear Seamount, 39°53′N, 67°26′W to 39°52′N, 67°23′W, Yankee 36 otter trawl, net depth: 1,489 m, R/V Delaware II cruise DE02–06, st. 46, coll. J. A. Moore, 29 July 2002 (preservation not recorded, not likely formalin).
YPM 27001, Bear Seamount, 39°55.22′N, 67°28.83′W to 39°54.24′N, 67°29.80′W, Yankee 36 otter trawl (1-h trawl), 1,826–2,008 m, R/V Delaware II cruise DE00–11, st. 17, coll. J. A. Moore, 5 December 2000 (frozen on board, then fixed in 70% ethanol).
YPM 27001 is a large bowl-shaped specimen, 40 cm in diameter, with a flattened top surface (Fig. 3a). YPM 28261 is smaller with a more inflated top surface (Fig. 3b). Cribriporal pores (0.5–1 mm in diameter) are on the sides, cribriporal to uniporal oscules on the top surface (0.5–1 mm in diameter); cortex is 1–2 mm (YPM 27001) or 1–1.5 mm (YPM 28261) thick. Cortex is white; the choanosome is also white, a bit creamer. YPM 28261 has parasitic Hyrrokkin sp. foraminifera (Fig. 3c) deeply settled in the cortex, only in the pore areas (Fig. 3b) (identification on pictures by T. Cedhagen, Aarhus University, Denmark).
Spicules, YPM 28261
(a) Oxeas I: length, 4,025 μm (n = 1); width, 25 μm (n = 1). (b) Oxeas II (= microxeas): mostly straight but sometimes slightly bent; length, 262–318.8–360 μm; width, 7.5–9.3–11 μm. (c) Orthotriaenes: rhabdome length, 2,825–6,642–7,920 μm (n = 10); width, 40–106–120 μm (n = 15); clad length, 230–690–1,000 μm (n = 10). (d) Anatriaenes: rhabdome length, >15 mm; width, 40–40.6-42 μm (n = 3); clad length, 260 μm (n = 1). (e) Promesotriaene: rhabdome width, 11 μm (n = 1); clad length, 260 μm (n = 1); central clad length, 200 μm (n = 1).
COI barcoding and mini-barcoding
We managed to sequence the universal Folmer barcoding fragment for YPM 27001 (Genbank no. KX982850), it is 100% identical to all other G. macandrewii sequenced previously (e.g., EU4422198) (Cárdenas et al. 2011, 2013): nine sequences from Norway (four), Spitsbergen (two), Porcupine Bank (one), Davis Strait (one) and Flemish Cap (one). The universal mini-barcode sequence of YPM 28261 was 100% identical to the first 130 bp of the Folmer fragment of G. macandrewii, this was the first blast hit.
157–2,012 m (Cárdenas et al. 2013; this study).
With its moderately thick cortex (1–2 mm), its very hairy sides and cribriporal pores and oscules, these specimens look like typical G. macandrewii. Furthermore, spicule measurements are perfectly in accordance with the description of the species (Cárdenas and Rapp 2015; Cárdenas et al. 2013). G. macandrewii was only collected in the Bear Seamount (seamount closest to the continental shelf, Fig. 1) but underwater pictures suggest it is also present in the Retriever Seamount (Fig. 2c), ~100 km from Bear Seamount (Fig. 1). Both of these seamounts are now protected as part of the Northeast Canyons and Seamounts Marine National Monument. Sightings in the Retriever Seamount were at 2,012 m depth, making it the deepest record for this species. The foraminifera could be the common parasitic Hyrrokkin sarcophaga Cedhagen 1994 described in the Northeast Atlantic on Geodia sponges, including G. macandrewii (Beuck et al. 2008; Cedhagen 1994) but genetic data are wanting to confirm this identification.
Geodia megastrella Carter, 1876
YPM 28870, Muir Seamount, 33°46.54′N, 62°34.29′W, DSV Alvin dive 3885, st. 1, 2,027 m, R/V Atlantis cruise AT07–35, coll. D. Scheirer and R. Waller, 3 June 2003 (fixed in formalin).
YPM 28891, Muir Seamount, 33°45.20′N, 62°45.10′W, DSV Alvin dive 3887, st. 5, 2,265 m, R/V Atlantis cruise AT07–35, coll. J. Adkins and L. Robinson, 6 June 2003 (fixed in formalin).
YPM 58540, Muir Seamount, 33°45.20′N, 62°45.10′W, DSV Alvin dive 3887, st. 5, 2,265 m, R/V Atlantis cruise AT07–35, coll. J. Adkins and L. Robinson, 6 June 2003 (fixed in formalin).
YPM 34730, Kelvin Seamount, 38°50.992′N, 63°55.572′W, DSV Alvin dive 3904, st. 208–1, 1,880 m, R/V Atlantis cruise AT08–01, coll. S. C. France and I. G. Babb, 16 July 2003 (fixed in formalin).
YPM 36027, Manning Seamount, 38°08.09′N, 61°06.965′W, ROV Hercules dive 6, St. MAN708, 1,718 m, R/V Ronald H. Brown cruise RB04–04, coll. J. A. Moore, 15 May 2004 (preservation not recorded).
YPM 46869, Picket Seamount, 39°39.14052′N, 65°56.600400′W, DSV Alvin dive 4162, st. PIC 104–1, 1,995 m, R/V Atlantis cruise AT12–01, coll. L. Mullineaux and S. Eltgroth, 28 October 2005 (fixed in formalin).
YPM 28870, 46869, 34730 and 58540 are large subspherical specimens. Diameters range from 8 cm (YPM 46869) to 20 cm (YPM 58540). YPM 28891 is more flattened (6 × 5 cm). All samples have one single preoscule opening (0.3–1.5 cm in diameter) on the top surface except for YPM 34730 that has two (Fig. 5b). Smaller preoscule openings (3–4 mm) have raised margins (YPM 36027). On the sides, cribriporal areas (2–3 mm in diameter) have characteristic ‘snowflake’ shapes (Fig. 5d). Specimens are not compressible with a very hard and thick cortex (1.5–3 mm). Surface is smooth, to human-skin-like, to beehive-like patterns. YPM 28891 and 58540 are growing on coral rubble; YPM 36027 is growing on dead Lophelia skeleton, while YPM 46869 was attached to the base of live Paragorgia. External color alive and in ethanol is brown to light brown. Internal color alive and in ethanol is cream (lighter than cortex).
Spicules, YPM 28870, unless stated otherwise.
(a) Oxeas I: straight or slightly bent, some are slightly centrotylote; length, 2,600–2,998–3,680 μm (n = 7); width, 35–46.8–60 μm (n = 7). (b) Oxeas II (= microxeas): straight or slightly bent, with very sharp tips; length, 225–372.4–570 μm; width, 3.5–6.8–7.5 μm. (c) Orthotriaenes: rhabdome length, 3,160–3,480 μm (n = 2); width, 90–97–110 μm (n = 10).
(d) Sterrasters: spherical to subspherical (Fig. 4b), 195–212.6–225 μm in diameter; thickness, 155–160 μm; sterrasters in the rest of the specimens are more elongated (sometimes lemon-shaped) (Fig. 4c). (e) Strongylasters: 5.0–7.2–10 μm in diameter. (f) Oxyasters I: 5–9 rough actines; diameter, 73–90.5–105 μm (Fig. 4b-c); oxyasters in YPM 34730, 28891 and 36027 have many oxyasters reduced to 3–2 actines, which often makes much larger oxyasters (diameter, 60–121.3–187 μm in YPM 34730) with actines up to 90 μm long. (g) Oxyasters II: thin rough actines; diameter, 15–29.4–50 μm. Anatriaenes and protriaenes not observed.
Identical universal mini-barcodes (130 bp) were obtained for three samples (out of six): YPM 028891, YPM 046869 and YPM 034730. Identical Depressio-minibarcodes (296 bp) were obtained for two samples: YPM 028891, YPM 046869. These Depressio-minibarcodes are 100% identical with a G. megastrella sequence from the Gulf of Cadiz (ZMAPOR 21231, Genbank no. HM592741) but have 1-bp difference with two other G. megastrella sequences from Scotland and Irving Seamount (south of the Azores) (Cárdenas et al. 2011). Two merged mini-barcode sequences (YPM 028891, 046869) were submitted to Genbank (KX982851–KX982852).
Spicule measurements and external morphology are perfectly in accordance with previous descriptions from the Mid-Atlantic Ridge and Madeira (Cárdenas and Rapp 2015; Topsent 1928). Lemon-shaped sterrasters have also been observed in MNHN-DT1298 from Madeira, 2380 m (Topsent 1928). Contrary to its sister species in the Depressiogeodia clade (the boreal G. barretti and the arctic G. hentscheli) (Cárdenas et al. 2011), this species is not known to form mass occurrences (i.e., sponge grounds). This species was sighted (Fig. 2a) and collected between 1,719 and 2,265 m depth on several NES (Picket, Kelvin and Manning) and Muir Seamount (Fig. 1). Although the Depressio-minibarcodes are identical to the COI sequence of G. megastrella ZMAPOR 21231, the external morphology and spicule sizes of the latter are slightly different from our specimens (and those from the Mid-Atlantic Ridge or Madeira), thus suggesting the presence of genetically cryptic species with identical COI in this already suspected species complex (Cárdenas et al. 2011). This is the first time that this typical deep-sea northeastern Atlantic Geodia is recorded on the northwestern side. This G. megastrella morphotype (identical to the specimens from Madeira and the Mid-Atlantic Ridge) can therefore be added to the growing list of deep-sea amphi-Atlantic boreo/arctic/temperate demosponges (Cárdenas et al. 2013; Cárdenas and Rapp 2015).
Geodia barretti Bowerbank, 1858
YPM 28886, Muir Seamount, 33°45.42′N, 62°36.06′W, DSV Alvin dive 3886, st. 1, 2,829 m, R/V Atlantis cruise AT07–35, coll. T. Shank and S. Eltgroth, 5 June 2003 (preservation not recorded, probably formalin).
Spherical, 6 cm in diameter, regular short hispidity, slightly compressible, light-brown external color, cream color inside (lighter), one elevated preoscule (3.5 mm in diameter), slightly flexible cortex = 1 mm, radial skeleton organization, Pores areas <1 mm, on the bottom half of the sphere. Dichotriaenes/pro(meso)triaenes/anatriaenes crossing the surface.
Spicules, YPM 28886
(a) Oxeas I: slightly bent, some are slightly centrotylote; length, 860–2,328–3,680 μm (n = 12); width, 16–34.9–50 μm (n = 10). (b) Oxeas II (= microxeas): straight or slightly bent; length, 262–470.2–600 μm; width, 5–7.6–17 μm. (c) Dichotriaenes: rhabdome length, 2,520–2,768–3,000 μm (n = 12); width, 110–126–140 μm (n = 11); protoclad length, 200–243-300 μm (n = 15); deuteroclad length, 200–284-360 μm (n = 15). (d) Anatriaenes: only observed at the surface, not measured. (e) Mesotriaenes: clads are sickle shaped; rhabdome length, 1,475 μm (n = 1); width, 5–12.3–17 μm (n = 3); clad length, 170–253–300 μm (n = 3); central clad length, 20–50–70 μm.
Microscleres (Fig. 4d):
(f) Sterrasters: spherical; 85–114.5–125 μm in diameter; thickness, 95–97 μm. (g) Strongylasters: 5–6.4–10 μm in diameter. (h) Oxyasters I: rough actines, a few have a single much longer actine (up to 72 μm long); diameter, 38–47.7–65 μm. (i) Oxyasters II: thin actines; diameter, 12.5–24.9–38 μm.
The universal mini-barcode and Depressio-minibarcode were both sequenced. The resulting merged sequence (Genbank no. KX982853) was 100% identical to the COI haplotype 1 of G. barretti (e.g., EU442195).
30–2,829 m (Cárdenas and Rapp 2013; this study)
Spicule measurements are in accordance with the description of the species (Cárdenas et al. 2013). A few differences are, however, noted. This specimen has the largest sterrasters (85–114.5–125 μm) measured to date for this species. Since there seems to be a relation between depth and size of sterrasters (Cárdenas and Rapp 2013), this may be related to the fact that this is the deepest record of G. barretti. Also, unlike previous observations in G. barretti, there is no clear size distinction between oxyasters I and II in this specimen; it is more of a continuum. Moreover, the large oxyasters with a single unusually long actine found here had never been observed in G. barretti before, or even in North Atlantic Geodia species. Finally, the relatively dark brown color and the hispidity of this specimen are also atypical for this species (Cárdenas et al. 2013). All these small differences suggest that the Muir Seamount may somehow represent a separate population. This is the western-most record of this species in the Atlantic and although no specimens were collected in the NES, its presence on the Muir Seamount suggests its presence in the neighboring NES. The carnivorous sponge Abyssocladia polycephalus Hestetun et al. 2016 was found growing on this specimen.
To test the use of the two mini-barcodes on old type material, we tried to get mini-barcodes from the dry holotype of Geodia barretti (NHM 18188.8.131.529) collected in 1855. Although DNA could not be detected in our extract, we succeeded in sequencing the COI universal mini-barcodes and the Depressio-minibarcodes (following the PCR protocols detailed above), thus obtaining a total of 416 bp from this 161-year-old type. The merged sequence, submitted to the Sponge Barcoding Project (SBP no. 1647, Genbank no. KX982854), was 100% identical to the COI haplotype 1 of G. barretti.
We report here the first records of G. macandrewii, G. barretti and G. megastrella in the NES area. The modeling of the distribution of boreo-arctic Geodia species by Howell et al. (2016) failed to predict the presence of boreal Geodia in the NES, which is probably an indication of the knowledge gaps pertaining to the distribution of deep-sea sponges. Geodia spp. seem highly abundant in this region with 698 sightings in the NES and 140 in the Corner Rise Seamounts (Cho 2008, p. 47). No large sponge grounds such as the ones observed off Newfoundland (Murillo et al. 2012) have been recorded from the NES so far, despite the presence of key boreal sponge ground species (G. barretti or G. macandrewii). Aggregations of different Geodia species are present (Fig. 2b, c) but their extent and density has not been measured.
This small collection suggests that the NES and Muir Seamount Geodia fauna include both boreal (G. barretti and G. macandrewii) and temperate species (G. megastrella). The mix of boreal and temperate species in the NES has been noticed for other groups such as fish (Moore et al. 2003b, 2003a; Quattrini et al. 2015), cephalopods (Shea et al. 2017) and octocorals (Cairns 2007; Quattrini et al. 2015; Watling et al. 2011). Moore et al. (2003b, 2003a) found that there is an area of overlap between the boreal fauna and temperate fauna along the slope of Georges Bank. The Deep Western Boundary Current (DWBC) along the continental slope of Georges Bank originates from the cold Labrador Current and actually runs at depths down to Cape Hatteras (Spall 1996; Moore et al. 2004). Other boreal/temperate Geodia species live in sympatry with G. barretti and G. macandrewii in the Flemish Cap/Grand Banks area: the boreal Geodia atlantica (Stephens, 1915), Geodia phlegraei (Sollas, 1880) and the temperate Geodia nodastrella Carter, 1876 (Cárdenas and Rapp 2015; Cárdenas et al. 2013). Therefore, we can expect to find these other species in the NES, should their ecological needs (species interactions, ecological conditions) be met there. Furthermore, the warm-core eddies off the Gulf Stream drop tropical species into the area. As a result, Bear Seamount’s fish and cephalopod fauna has a mix of boreal, temperate and tropical species (Moore et al. 2003a; Shea et al. 2017). Although pelagic animals are obviously very mobile and require different ecological interactions/conditions than sponges, this opens up the possibility of also finding subtropical Geodia species in the NES. For instance, the type locality of the temperate/subtropical Geodia pachydermata is nearby (in the Bermuda, 250 km from Muir Seamount), so we could expect this species to be present in this area. These results also highlight the overlap between the biogeographic lower bathyal provinces BY2 (Northern Atlantic Boreal, including the Grand Banks and Flemish Cap) and BY4 (North Atlantic, including the NES) (Watling et al. 2013) in this region.
Although our specimen of G. barretti from Muir Seamount presented small morphological differences with typical specimens, G. macandrewii and G. megastrella specimens were quite typical of the species. This collection is however too small to deduce anything about local endemism on seamounts. Genetic studies on other benthic animals (octocorals and antipatharians) from the NES and Corner Seamounts suggest that populations from the individual seamounts are not isolated (Thoma et al. 2009) so it may be similar for sponges.
With a full-length barcode (= Folmer barcode) the three species from this study could potentially be identified unambiguously (Cárdenas et al. 2011). However, because of the degraded DNA, obtaining a full-length barcode was only possible for the only specimen originally frozen on board: YPM 27001 (G. macandrewii). Sequencing of the universal mini-barcode (= first 130 bp of the Folmer barcode) was easier (five sequences obtained out of eight specimens) and succeeded in identifying unambiguously G. macandrewii but not G. barretti and G. megastrella. The latter two species have identical universal mini-barcodes, as do all Geodia species that belong to the Depressiogeodia clade (G. barretti, G. hentscheli and G. megastrella sensu lato).
Although restricted to a few species, our results therefore show that, as expected, identification of sponges is not as accurate with the COI universal mini-barcodes as with the COI full-length barcode. Knowing that sponge COI barcoding is already limited due to its slow evolution (Schuster et al. 2017, and references within) up to the point that it cannot discriminate close species (Addis and Peterson 2005; Cárdenas and Rapp 2012; Carella et al. 2016), the mini-barcode worsens the problem. And yet, in our small study, the universal mini-barcode unambiguously identified the Geodia genus, which could already be of tremendous help for taxonomists, ecologists and other end-users of sponge barcoding. In some cases, we show that it can even identify to the species level (G. macandrewii).
The Depressio-minibarcode (= last 296 bp of the Folmer barcode) performed as well as the full-length barcode since it could by itself identify unambiguously each of these Geodia species. It was actually variable enough to also discriminate the different G. megastrella and G. barretti haplotypes. Future work should determine if these results—Depressio-minibarcode was more variable than the universal mini-barcode—can be confirmed for other sponges. The primer Tetract-minibarR1 is positioned in a moderately conserved part of COI, with no known mitochondrial intron insertion sites (Schuster et al. 2017). We show here that the primer pair LCO/Tetract-minibarR1 worked for Geodia species, but it should work for all Tetractinellida: we have already successfully tested it on several tetractinellid genera (Vulcanella, Pachastrella, Rhabdastrella, Ecionemia, Erylus, Caminus, Stelletta, Antarctotetilla, Cinachyrella, Tetilla and Craniella). Primer Depressio398F is specific to the Depressiogeodia clade but it appears to work occasionally on other Geodia species (data not shown).
One important advantage of COI mini-barcodes is that they do not require yet another sponge barcoding database, which would take years to build; they take advantage of the already substantial COI sponge barcode database in Genbank and the Sponge Barcoding Project (http://www.palaeontologie.geo.uni-muenchen.de/SBP). More generally, one major benefit with mini-barcodes is that one can barcode specimens with degraded DNA, such as the ones from this study. We managed to get sequences of 100–300 bp from formalin-fixed specimens collected 11–14 years ago. This opens the possibility to use numerous outstanding museum collections, for which the sponge specimens have unfortunately been in formalin (e.g., MAR-Eco 2004 collection, ZMBN; BIOFAR 1988–1990 collection, ZMUC) or simply bulk-fixed in 70% ethanol (this is the case for many recent collections at the MNHN). It has been previously suggested that, in Vertebrates at least, tissue lysis is the main obstacle in obtaining DNA from formaldehyde-exposed tissues due to the DNA crosslinking to the surrounding tissue, making complete lysis difficult (Zimmermann et al. 2008). In our case, we did not observe any problem to completely dissolve the formalin-fixed sponge pieces in our lysis buffer. However, the amounts of DNA we extracted using a standard kit were indeed extremely low (usually <25 pg/μl).
Mini-barcodes would also be strong assets to easily sequence old museum material, especially type material (Hajibabaei et al. 2006; Hajibabaei and McKenna 2012). In this study, we succeeded in obtaining the two mini-barcodes from the 161-year-old dry holotype of Geodia barretti (NHM 18184.108.40.2069), collected in 1855. According to the World Porifera Database (van Soest et al. 2017), 44% of all sponge species (accepted and unaccepted) were described during the eighteenth and nineteenth centuries; another 47% of all species were described in the twentieth century. This means that 91% of all sponge species have type material that predate the year 2000, a time when sponge molecular phylogenetics was just emerging and sponge taxonomists seldom thought of properly preserving the DNA of their specimens. Consequently, this means that 91% of sponge types probably have degraded DNA. Even though it seems possible to sequence full-length barcodes even for century-old types (Erpenbeck et al. 2015), this is rather the exception than the rule. On the other hand, we foresee that obtaining COI and 28S mini-barcodes from reference specimens will certainly be easier and therefore more common, which would drastically raise the level of confidence users will have in the sponge barcoding database. Additionally, these mini-barcodes may solve a plethora of phylogenetic and taxonomical questions (e.g., Erpenbeck et al. 2015). Furthermore, if one is not satisfied with the short universal mini-barcode, its sequence is a prerequisite to try to get the full-length barcode, by primer walking for instance.
Many thanks to Eric A. Lazo-Wasem (senior collections manager, Yale Peabody Museum of Natural History) for sharing this material, for his diligent efforts to answer our queries and for taking pictures of the specimens. The collection of specimens was made possible by generous funding provided by the NOAA Ocean Exploration program (NA03OAR4600116), NOAA National Marine Fisheries Service (for ship time on RV Delaware II), NOAA National Undersea Research Program (NA05OAR4301001), and NSF (OCE-0096373). We would like to thank J. Moore’s colleagues in the Mountains in the Sea and Deep Atlantic Stepping Stones Research Groups: J. Adkins, P. Auster, S. France, I. Babb, L. Mullineaux, K. Scanlon, T. Shank, M. Vecchione, and L. Watling and for their help in securing the necessary funding and ship time to allow us to explore north-western Atlantic seamounts. Our sincere thanks to the captains and crew of the RV Atlantis and the NOAA ships Delaware II and Ronald H. Brown, who together with the skillful pilots of the DSV Alvin and ROV Hercules, made it possible to collect high quality imagery and specimens from great depths. We thank Cécile Jolly (EBC, Uppsala University) for assistance using the 2200 TapeStation and Raphaël Cárdenas (Gluntens Montessoriskola, Uppsala) for help measuring the specimens. This work has received funding from an Inez Johansson grant (HT2014, Uppsala University, Sweden) and the European Union’s Horizon 2020 research and innovation program through the SponGES project (grant agreement no. 679849).
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