Research Article |
Corresponding author: Melissa J. Betters ( melissajbetters@gmail.com ) Academic editor: Eike Neubert
© 2024 Melissa J. Betters, Erik E. Cordes.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Betters MJ, Cordes EE (2024) New records of Provanna (Gastropoda, Provannidae) from the Costa Rica Margin and an identification key for the genus. ZooKeys 1189: 1-32. https://doi.org/10.3897/zookeys.1189.109734
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Consistent species identification is foundational to biological research and requires coordination among a diversity of researchers and institutions. However, such consistency may be hindered for rare organisms where specimens, identification resources, and taxonomic experts are few. This is often the case for deep-sea taxonomic groups. For example, the deep-sea gastropod genus Provanna Dall, 1918 is common at chemosynthetic sites throughout the world’s oceans, yet no formal guide to these species has yet been produced. Recent exploration has recovered new specimens of Provanna from hydrocarbon seeps off the Pacific Costa Rica Margin. The current work assesses the species identity of these specimens using shell morphology, radular morphology, and genetic barcoding (mitochondrial CO1 and nuclear H3). Records of occurrence for P. laevis Warén & Ponder, 1991, P. ios Warén & Bouchet, 1986, and P. pacifica Warén & Bouchet, 1986 are herein presented from the Costa Rica Margin. A critical taxonomic review of the 29 extant species within this genus was conducted and their genetic, morphological, and biogeographical distinction assessed. In this review, genetic and morphological support was found for nearly all current species delineations except for P. glabra
Gastropoda, identification, species delimitation, systematics, taxonomy
Consistent species identification is foundational to biological research. Studies of populations, communities, and ecosystems all rely on authors from a wide range of backgrounds and locations coordinating species definitions. This is particularly salient for the global endeavor of deep-sea research, where many species are recent discoveries. As many regions of the ocean remain unexplored, taxonomic characterization of marine invertebrates are hindered by a lack of collections, occurrence records, identification resources, and taxonomic experts (
Throughout the world’s oceans, ecosystems reliant on chemosynthetic activity, such as hydrothermal vents and hydrocarbon seeps, are hotspots for productivity on the ocean floor, hosting an anomalously high biomass community consisting of numerous endemic species (
The current work centers on aa genus of Abyssochrysoid snails Provanna (Dall, 1918), presenting new records, a taxonomic review, and a new identification key for its species. Provanna occur worldwide and are endemic to chemosynthetic environments (
Species of Provanna, like other deep-sea gastropods, may be distinguished by their shell and radular morphology, making a morphology-based identification key useful. All Provanna share certain characteristics that distinguish the genus. Specimens have small, turbinate, dextral shells, a thin periostracum, no umbilicus, and usually no more than 2–3 shell whorls intact, regardless of size. They are never wider than they are tall and their apertures have a distinct shape; They are rarely circular or ovate. Rather, the columellar lip typically curves inwards near the bottom of the shell, such that it forms a near-right angle with the lower lip (see Fig.
In the present study, we present formal records of Provanna from hydrocarbon seeps at the Costa Rica Margin that were sampled from 700 to 2000 meters depth. These sites were sampled during three cruises from 2017–2019, representing one of the most intensive sampling efforts in this region to date. The hydrocarbon seepage in this region is driven by the subduction of the Cocos Plate beneath the Caribbean plate (
Specimens of Provanna were obtained from one of six sites at the Pacific Costa Rica Margin (CRM) during research expeditions conducted from 2017 to 2019 (Fig.
Summary of hydrocarbon seep sites sampled at the Costa Rica Margin and their associated species yield. Abbreviations in cruise identities are defined as follows: FK = R/V ‘Falkor’ cruise number, AT = R/V ‘Atlantis’ cruise number. Abbreviations: SD = ROV ‘Subastian’ dive number, AD = HOV ‘Alvin’ dive number. *Previously identified as P. goniata.
Seep site | Number of specimens | Species composition | GPS coordinates | Depth (m) | Cruise ID | Dive ID |
---|---|---|---|---|---|---|
Jaco Summit | 6 | P. laevis (100%) | 9.174°N, 84.800°W | 740–760 | FK19-0106 AT37-10 AT37-13 | SD213 AD4874 AD4912 AD4913 AD4914 |
Jaco Scar | 180 | P. ios (100%)* | 9.115°N, 84.836°W | 1800–2000 | AT42-03 | AD4971 AD4973 AD4977 AD4989 |
FK19-0106 | SD214 | |||||
Quepos Seep | 6 | P. pacifica (100%) | 8.922°N, 84.305°W | 1000–1100 | AT37-13 | AD4924 |
The Thumb | 815 | P. laevis (100%) | 9.049°N, 84.354°W | 1071–1075 | FK19-0106 | SD217 |
Mound 12 | 803 | P. laevis (100%) | 8.930°N, 84.313°W | 900–1050 | AT37-13 | AD4907 AD4910 AD4917 |
AT42-03 | AD4974 AD4978 AD4984 AD4985 AD4987 | |||||
Mound 11 | 5 | P. lomana (40%), P. pacifica (60%) | 9.031°N, 84.619°W | 1300–1500 | AT42-03 | AD4988 |
All morphological characters and measurements are defined in Fig.
Definitions for selected terminology used to describe morphological characters.
Aperture | The opening of the shell from which the gastropod body would protrude |
Axis of coiling | The imaginary line that runs from the top of a shell’s spire to the tip of its base around which the shell is coiled |
Axial sculpture | The sculpturing of the shell running parallel to the axis of coiling |
Growth lines | Fine transverse lines marking shell growth. They are distinguished from axial sculpturing in that they are not raised or grooved. |
Sculpture | Three-dimensional, linear ornamentation on the outer surface of the shell. These rise away from the shell surface |
Sculptural element | Knob-, bead-, or spike-like protrusions that occur at intersections of the axial and spiral sculptures and that are raised higher than either sculpture. Note: If a Provanna shell has structural elements, it will typically have both an axial and spiral sculpture. |
Body whorl margin | The length between the posterior end of the aperture and the previous suture line |
Spiral sculpture | The sculpturing of the shell running perpendicular to the axis of coiling |
Suture | Where the whorls of the shell are fused, including where the aperture is fused with the body whorl |
Whorl | One complete revolution of shell growth |
Summary of morphological characteristics for the type specimens of each Provanna species.
Species | Axial ribs on body whorl | Spiral ribs on body whorl | Relative strength of ribs on body whorl | Sculptural elements | Axial body sculpture extends to… | |
P. abyssalis Okutani & Fujikura, 2002 | 0 | 0 | NA | Absent | NA | |
P. admetoides Warén & Ponder, 1991 | 35–45 | 2–3 | Variable | Minor spines/Absent | Posterior end of aperture | |
P. annae Nekhaev, 2023 | 0 | 0 | NA | Absent | NA | |
P. beebi |
>20 | 0–6 | Spiral > Axial | Beaded/ Absent | Anterior end of shell | |
P. buccinoides Warén & Bouchet, 1993 | 10–20 | 3–4 | Spiral < Axial | Nodules | Posterior end of aperture | |
P. chevalieri Warén & Bouchet, 2009 | 10–20 | 0–3 | Spiral < Axial | Absent | Mid-body whorl | |
P. cingulata |
0 | 4–6 | Spiral > Axial | Absent | NA | |
P. clathrata |
10–20 | 3–5 | Variable | Nodules/ Minor Spines | Posterior end of aperture | |
P. cooki |
0 | 0–5 | Spiral > Axial | Absent | NA | |
P. exquisita Chen & Watanabe, 2022 | 14–18 | 2–3 | Spiral > Axial | Major Spines/Keel | Posterior end of aperture | |
P. fenestrata |
16–20 | 1–2 | Variable | Nodules/ Absent | Posterior end of aperture | |
P. glabra |
0 | 0 | NA | Absent | NA | |
P. goniata Warén & Bouchet, 1986 | 15–20 | 2–3 | Spiral > Axial | Major Spines | Posterior end of aperture | |
P. ios Warén & Bouchet, 1986 | 15 | 2 | Spiral > Axial | Minor Spines | Posterior end of aperture | |
P. kuroshimensis |
0 | 0 | NA | Absent | NA | |
P. laevis Warén & Ponder, 1991 | 0 | 0 | NA | Absent | NA | |
P. lomana Warén & Bouchet, 1986 | 10–20 | 0 | Spiral < Axial | Absent | Posterior end of aperture | |
P. lucida |
0 | 0–3 | Spiral > Axial | Absent | NA | |
P. macleani Warén & Bouchet, 1989 | 10–20 | 4–5 | Spiral > Axial | Absent | Posterior end of aperture | |
P. muricata Warén & Bouchet, 1986 | 14–16 | 1–2 | Spiral < Axial | Nodules/ Minor Spines | Posterior end of aperture | |
P. nassariaeformis Okutani, 1990 | 20–25 | 3–5 | Spiral = Axial | Beaded | Anterior end of shell | |
P. pacifica Warén & Bouchet, 1986 | 12–16 | 2–3 | Spiral > Axial | Nodules/ Minor Spines | Posterior end of aperture | |
P. reticulata Warén & Bouchet, 2009 | 0–15 | 2–4 | Spiral = Axial | Minor Spines | Posterior end of aperture | |
P. sculpta Warén & Ponder, 1991 | 15 | 3 | Spiral < Axial | Beaded | Posterior end of aperture | |
P. segonzaci Warén & Ponder, 1991 | 10–20 | 2–3 | Spiral < Axial | Nodules/ Minor Spines | Posterior end of aperture | |
P. shinkaiae Okutani & Fujikura, 2002 | 10–20 | 2–3 | Spiral > Axial | Major Spines | Posterior end of aperture | |
P. stephanos |
10–20 | 2–3 | Spiral > Axial | Major Spines/Keel | Posterior end of aperture | |
P. subglabra |
0 | 0 | NA | Absent | NA | |
P. variabilis Warén & Bouchet, 1986 | 0–20 | 1–3 | Spiral > Axial | Nodules/ Absent | Posterior end of aperture | |
Species | Basal spiral ribs | Width / Length | Depth of suture | Aperture shape description | Central tooth width | Central tooth cusp |
P. abyssalis Okutani & Fujikura, 2002 | Absent | 0.5 | Constricted | Globose | Typical | Long, triangular |
P. admetoides Warén & Ponder, 1991 | Present | 0.61 | Moderate | Fusiform | Very narrow | Very truncated |
P. annae Nekhaev, 2023 | Absent | 0.6 | Constricted | Globose | Typical | Long, triangular |
Species | Basal spiral ribs | Width / Length | Depth of suture | Aperture shape description | Central tooth width | Central tooth cusp |
P. beebi |
Present | 0.59 | Moderate | Fusiform/ Semicircle | Broad | Blunt, truncated |
P. buccinoides Warén & Bouchet, 1993 | Present | 0.63 | Moderate | Globose | Broad | Blunt, truncated |
P. chevalieri Warén & Bouchet, 2009 | Present | 0.55 | Constricted | Globose | Broad | Very short, triangular |
P. cingulata |
Absent | 0.61 | Constricted | Globose | Broad | Short, triangular |
P. clathrata |
Present | 0.61 | Constricted | Fusiform | Typical | Long, triangular |
P. cooki |
Absent | 0.57 | Constricted | Fusiform | Broad | Triangular |
P. exquisita Chen & Watanabe, 2022 | Present | 0.55 | Constricted | Semicircular | Typical | Triangular |
P. fenestrata |
Present | 0.59 | Moderate | Variable | Typical | Triangular |
P. glabra |
Absent | 0.6 | Flat | Globose | Typical | Triangular, blunt |
P. goniata Warén & Bouchet, 1986 | Present | 0.59 | Moderate | Globose/ Fusiform | Typical | Long, triangular |
P. ios Warén & Bouchet, 1986 | Variable | 0.54 | Constricted | Fusiform/ Semicircle | NA | Long, triangular |
P. kuroshimensis |
Absent | 0.58 | Flat | Fusiform | Typical | Long, triangular |
P. laevis Warén & Ponder, 1991 | Absent | 0.56 | Flat | Variable | Typical | Short, triangular |
P. lomana Warén & Bouchet, 1986 | Present | 0.55 | Moderate | Globose | Typical | Long, triangular |
P. lucida |
Absent | 0.59 | Constricted | Globose | Typical | Short, triangular |
P. macleani Warén & Bouchet, 1989 | Present | 0.61 | Moderate | Fusiform | Very narrow | Very truncated |
P. muricata Warén & Bouchet, 1986 | Present | 0.56 | Constricted | Globose | Typical | Triangular |
P. nassariaeformis Okutani, 1990 | Present | 0.7 | Flat | Fusiform | Broad | Triangular, blunt, truncated |
P. pacifica Warén & Bouchet, 1986 | Present | 0.61 | Moderate | Fusiform | Very narrow | Very truncated |
P. reticulata Warén & Bouchet, 2009 | Present | 0.57 | Moderate | Fusiform | Broad | Blunt, truncated |
P. sculpta Warén & Ponder, 1991 | Present | 0.55 | Moderate | Fusiform | Typical | Long, triangular |
P. segonzaci Warén & Ponder, 1991 | Present | 0.59 | Constricted | Fusiform | Typical | Triangular |
P. shinkaiae Okutani & Fujikura, 2002 | Present | 0.51 | Moderate | Semicircle | Typical | Long, triangular |
P. stephanos |
Present | 0.61 | Flat | Globose | Typical | Short, triangular |
P. subglabra |
Absent | 0.61 | Flat | Fusiform | Typical | Long, triangular |
P. variabilis Warén & Bouchet, 1986 | Variable | 0.55 | Moderate | Globose | Typical | Long, triangular |
Species | Central tooth anterior ridge | First lateral tooth cusps | First lateral major cusp | First lateral major cusp shape | First lateral buttress angle | Marginal tooth cusps |
P. abyssalis Okutani & Fujikura, 2002 | Concave | 6–7 | 2nd | Triangular, fused with first | Right | 9–10 |
P. admetoides Warén & Ponder, 1991 | Rounded | 3–4 | 2nd | Spatulate | Obtuse | Alternating 7 or 14+ |
P. annae Nekhaev, 2023 | Concave | 3–4 | 2nd | Long, lobate | Right | 7–9 |
P. beebi |
Flat | 4–5 | 2nd | Truncated, lobate | Absent | 13–17 |
P. buccinoides Warén & Bouchet, 1993 | Rounded/Flat | 7 | Fourth | Very truncated, lobate | Absent | ~30 |
P. chevalieri Warén & Bouchet, 2009 | Variable | 4–5 | 2nd | Very truncated, lobate | Sloping/ Absent | 13–18 |
P. cingulata |
Round/Flat | 4–5 | 3rd or 4th | Rhomboid | Absent | 15–18 |
P. clathrata |
Concave | 4–5 | 2nd | Long, triangular | Right/ Acute | 9–10 |
P. cooki |
Concave | 5–6 | 2nd | Long, lobate | Obtuse | 11–14 |
Species | Central tooth anterior ridge | First lateral tooth cusps | First lateral major cusp | First lateral major cusp shape | First lateral buttress angle | Marginal tooth cusps |
P. exquisita Chen & Watanabe, 2022 | Concave | 4–5 | 2nd | Truncated, lobate | Right/ Obtuse | 20–24 |
P. fenestrata |
Concave | 4–5 | 2nd | Long, triangular | Right | 9–10 |
P. glabra |
Concave | 4–5 | 2nd | Long, lobate | Right/ Acute | 8–12 |
P. goniata Warén & Bouchet, 1986 | Concave | 5–6 | 2nd | Long, triangular | Right/ Acute | 15–25 |
P. ios Warén & Bouchet, 1986 | Concave | 4–5 | 2nd | Long, triangular | Right/ Acute | 15–25 |
P. kuroshimensis |
Concave | 4–5 | 2nd | Long, lobate | Right | 10–13 |
P. laevis Warén & Ponder, 1991 | Concave | 4–5 | 2nd | Truncated, lobate | Acute | 15–20 |
P. lomana Warén & Bouchet, 1986 | Concave | 4–5 | 2nd | Long, triangular | Acute | Alternating 7 or 14+ |
P. lucida |
Concave | 4–5 | 2nd | Long, triangular | Right/ Acute | 13–15 |
P. macleani Warén & Bouchet, 1989 | Rounded | 3–4 | 2nd | Spatulate | Sloping/ Absent | 15–20 |
P. muricata Warén & Bouchet, 1986 | Concave | 4–5 | 2nd | Lobate | Sloping/ Obtuse | 15–20 |
P. nassariaeformis Okutani, 1990 | Concave/Flat | 4–5 | 2nd | Truncated, lobate | Absent | 15–20 |
P. pacifica Warén & Bouchet, 1986 | Rounded | 3 | 2nd | Lobate/Spatulate | Sloping/ Obtuse | 5–7 |
P. reticulata Warén & Bouchet, 2009 | Concave | 2–3 | 2nd | Truncated, lobate | Absent | 15–20 |
P. sculpta Warén & Ponder, 1991 | Concave | 3–5 | 2nd | Long, triangular | Acute | 15–20 |
P. segonzaci Warén & Ponder, 1991 | Concave | 5–7 | 2nd | Multilobate | Right/ Obtuse | 15–20 |
P. shinkaiae Okutani & Fujikura, 2002 | Concave | 2–5 | 2nd | Long, lobate | Acute | 10–14 |
P. stephanos |
Concave | 4–5 | 2nd or 3rd | Long, triangular, blunt | Obtuse | 12–14 |
P. subglabra |
Concave | 4–5 | 2nd | Long, triangular | Right/ Obtuse | 15–20 |
P. variabilis Warén & Bouchet, 1986 | Concave | 4–5 | 2nd | Long, triangular | Acute | Alternating 7 or 14+ |
Visual definitions of morphological characters and measurements used in the study A shell morphological characters B informative measurements assessed for our own specimens C radular terminology and morphological characters. Abbreviations: SW: Shell Width, SL: Truncated Shell Length, GL: Maximum Granule Length, AL: Aperture Length, AW: Aperture Width.
To begin identifying the specimens from the CRM, they were first sorted into distinct morphotypes. Representatives from the full geographic, temporal, and size range of each morphotype were then selected for detailed morphological assessment. The following characters were measured for each specimen: Shell width (mm), truncated shell length (measured from the right, posterior tip of the penultimate whorl to the lowest point of the aperture (mm)), aperture length (mm), aperture width (mm), number of basal ribs (counted), relative shell texture (maximum granule length on the body whorl / truncated shell length), aperture roundness (width / length), and shell roundness (width / length). Truncated shell length was used as most Provanna lack any whorl past the penultimate whorl. Measurements of characters were taken from photographs captured by a mounted AmScope microscope adapter camera attached to a standard dissection microscope (Leica S6D, Leica Microsystems GmbH). A standardized 1-mm marker was present in every photo to allow for standardized measurements. Specimens were kept submerged in > 95% ethanol while images were taken. The line measurement tool within AmScope was used to measure morphological characters. To identify any potential collinearity among shell morphological characters, Pearson correlation coefficients (PCC) were calculated using the package Ggally (
To characterize the radulae of each morphotype, we performed the following protocol. First, the body whorl of the shell was punctured using a sharp probe. The whole animal was then incubated in a 1.5 mL microcentrifuge tube containing a 10% solution of proteinase-k for 5–15 min at 56 °C. Incubation was monitored and terminated once tissue was visibly loose and degraded, but not fully digested. The microcentrifuge tube was removed from the heat source, pulse-vortexed three times, and then its contents were rinsed into a clean glass petri dish using deionized (DI) water. Under a dissection scope, the radular ribbon was identified, extricated from any remaining soft tissue, and moved to another clean glass petri dish containing DI water to further dilute the proteinase-k solution and prevent further breakdown of the radular ribbon. Silicon wafer chips cut into ~ 1 cm3 squares were used as mounting substrate for scanning electron microscopy. To mount the radula, a very small droplet of DI water was placed onto a chip. The radula was then placed into this water droplet and manipulated under a light microscope into a flat, teeth-up position using forceps or a sharp probe. Manipulation was most successful when the radula was wet but not submerged. The radula’s position was monitored and adjusted under a light microscope while the water was allowed to evaporate. Once dry, radulae naturally adhered to the chip’s surface and were then stored dry until imaging. Scanning electron microscopy was undertaken using a QuantaTM 450 FEG scanning electron microscope (FEI 2012) in its low-vacuum setting at Temple University College of Engineering’s Nano Instrumentation Center. High-quality images were obtained without sputter coating. Tentative morphological identities were then ascribed to our specimens.
To confirm the morphological identifications, the cytochrome oxidase 1 (CO1) mitochondrial gene and the histone 3 (H3) nuclear gene were sequenced. Tissue was obtained by pulling aside the operculum and pinching off a small sample of tissue from the foot (approximately 1 mm3). This tissue was then digested and its DNA extracted using a Qiagen Blood and Tissue DNA Extraction kit (QIAGEN, Valencia, CA). Extracted DNA was quantitated using a Nanodrop 2000 spectrophotometer. DNA was kept frozen at -20 °C following extraction. A 710 base pair (bp) section of the CO1 gene was targeted for sequencing using the primers LCO1490/HCO2198 and polymerase chain reaction protocol put forth by
For all phylogenetic analyses, sequences were input and aligned using ClustalW embedded within the MEGA-X environment (v. 10.0.1;
To verify inclusion within the genus Provanna, we assessed our novel sequences in relation to other Abyssochrysoids including species in the genera Abyssochrysos (Tomlin, 1927), Cordesia (Warén & Bouchet, 2009), Rubyspira (
To assess the robustness of current species delimitations within the genus, we calculated the average pairwise sequence divergence (APD) across CO1 sequences for Provanna. All sequences with verified species identities were included; Sequences with tentative or unknown species identities were excluded. Our novel sequences were assigned to their hypothesized species identities. All sequences were aligned using ClustalW embedded within MEGA-X and assessed using a Tamura 3-parameter substitution model (
Using the conclusions drawn from the preceding sections, a taxonomic key for all genetically supported, extant species of Provanna was constructed. A polytomous key was chosen as the format to capture the natural variation found in Provanna shells (Fig.
. Examples of Provanna shell morphological variety A P. kuroshimensis, no sculpturing, growth lines present, flattened suture B–F constricted suture: B P. cooki, spiral sculpture only, no sculptural elements C P. chevalieri, axial sculpture only, no sculptural elements D–F both axial and spiral sculpturing: D P. fenestrata, sculptures about equal in strength, no sculptural elements E P. clathrata, axial sculpture stronger than spiral, blunt, sloping nodules F P. reticulata, spiral sculpture stronger than axial, minor spines.
Superfamily Abyssochrysoidea
Family Provannidae
Genus Provanna (Dall, 1918)
Costa Rica • 25 specimens; Costa Rica Margin, Mound 12; 8.930°N, 84.313°W; 999 m; 22 May 2017; Lisa Levin, Charlotte Seid leg.; ALVIN Dive 4907, from wood; Scripps Benthic Invertebrate Collection (SBIC) M16112. 11 specimens; Costa Rica Margin, Mound 12; 8.930°N, 84.313°W; 1004 m; 25 May 2017; Greg Rouse, Todd Litke leg.; ALVIN Dive 4910, from rock; SBIC M16104 and M16106. 16 specimens; Costa Rica Margin, Mound 12; 8.929°N, 84.315°W; 964 m; 1 June 2017; Greg Rouse, Ben Moran leg.; ALVIN Dive 4917, from mussel shells; SBIC M16176. 89 specimens; Costa Rica Margin, Mound 12; 8.930°N, 84.313°W; 1003 m; 20 October 2018; Lisa Levin, Kyle Metcalfe leg.; ALVIN Dive 4974, from mussel shells; SBIC M16765. 78 specimens; Costa Rica Margin, Mound 12; 8.931°N, 84.313°W; 1004 m; 24 October 2018; Erik Cordes, Melissa Betters leg.; ALVIN Dive 4978, from mussel shells. 104 specimens; Costa Rica Margin, Mound 12; 8.931°N, 84.313°W; 1002–1004 m; 30 October 2018; Erik Cordes, Melissa Betters leg.; ALVIN Dive 4984, from mussel shells. 5 specimens; Costa Rica Margin, Mound 12; 8.930°N, 84.313°W; 1001 m; 31 October 2018; Erik Cordes, Melissa Betters leg.; ALVIN Dive 4985, from mussel shells. 475 specimens; Costa Rica Margin, Mound 12; 8.930°N, 84.312–84.313°W; 1002–1007 m; 2 November 2018; Erik Cordes, Melissa Betters leg.; ALVIN Dive 4987, from tubeworms. 6 specimens; Costa Rica Margin, Jaco Summit; 9.174°N, 84.800°W; 742 m; 6 January 2019; Greg Rouse, Allison Miller leg.; SUBASTIAN Dive 213, from wood; SBIC M17030. 793 specimens; Costa Rica Margin, The Thumb; 9.049°N, 84.354–84.394°W; 1071–1075 m; 10 January 2019; Erik Cordes, Melissa Betters leg.; SUBASTIAN Dive 217, from mussel shells. 22 specimens; Costa Rica Margin, The Thumb; 9.049°N, 84.354–84.394°W; 1071–1075 m; 10 January 2019; Erik Cordes, Melissa Betters leg.; SUBASTIAN Dive 217, from tubeworms.
The range of P. laevis is here expanded to three hydrocarbon seep locations at the CRM: Mound 12, Jaco Summit, and The Thumb. Their known distribution in the Eastern Pacific Ocean ranges from the Juan de Fuca Ridge to the Costa Rica Margin. Their known depth distribution in the Eastern Pacific Ocean is between 700–2000 m (Table
Summary of biogeographic information for each known species of Provanna. S = Seep, V = Vent, F = Organic Fall. Note that P. glabra is herein synonymized with P. laevis and P. goniata is herein synonymized with P. ios.
Species | Region(s) | Localities | Depth (m) | Habitat | Citations |
---|---|---|---|---|---|
P. abyssalis Okutani & Fujikura, 2002 | W Pacific | Japan Trench | 5379 | S |
|
P. admetoides Warén & Ponder, 1991 | Gulf of Mexico | Off St. Petersburg, Gulf of Mexico | 624–631 | S |
|
P. annae Nekhaev, 2023 | N Pacific | Piip Volcano, Bering Sea | 387–472 |
|
|
P. beebi |
Caribbean Sea | Beebe Vent Field, Mid-Cayman Spreading Center | 4956–4972 | V |
|
P. buccinoides Warén & Bouchet, 1993 | W Pacific | Hine Hina, Lau Basin; North Fiji Basin | 1900–2765 | V |
|
P. chevalieri Warén & Bouchet, 2009 | E Atlantic | Regab, off West Africa | 3150 | S |
|
P. cingulata |
W Pacific | Shinkai Seep Field, Mariana Forearc | 5687 | S |
|
P. clathrata |
W Pacific | Irabu Knoll, Hatoma Knoll, Yaeyama Knoll, Okinawa Trough; Haima seep, South China Sea; Manus Basin | 1385–2190 | V,S |
|
P. cooki |
Southern | East Scotia Ridge, Southern Ocean | 2396–2639 | V |
|
P. exquisita Chen & Watanabe, 2022 | W Pacific | Eifuku Volcano, Mariana Arc | 1606 | V |
|
P. fenestrata |
W Pacific | Crane, Tarama Hill, Okinawa Trough; Sakai vent field; Haima seep, South China Sea | 1385–1973 | V,S |
|
P. ios Warén & Bouchet, 1986 (Synonymous with: P. goniata Warén & Bouchet, 1986) | E Pacific | 17 S, 13 N, 21 N, EPR; Guaymas Basin, Gulf of California; Galapagos Rift Zone; Costa Rica Margin | 2000–2616 | V,S |
|
P. kuroshimensis |
W Pacific | Kuroshima Knoll, off Okinawa | 644 | S |
|
P. laevis Warén & Ponder, 1991 (Synonymous with: P. glabra |
W & E Pacific | Guaymas Basin, Gulf of California; Juan de Fuca; Oregon Margin; Off Hatsushima, Sagami Bay; Minami-Ensei Knoll, Iheya Ridge, Okinawa Trough; Costa Rica Margin | 500–2004 | V,S |
|
P. lomana Warén & Bouchet, 1986 | E Pacific | Off San Diego, off Point Dume, California; Oregon Margin; Off San Nicolas | 450–1200 | V,F |
|
P. lucida |
W Pacific | Minami-Ensei Knoll, Okinawa Trough | 701 | V |
|
P. macleani Warén & Bouchet, 1989 | E Pacific | Oregon Margin | 2750 | F | Warén and Ponder 2001 |
P. muricata Warén & Bouchet, 1986 | E Pacific | 21 N, East Pacific Rise; Galapagos Rift | 2450–2615 | V |
|
P. nassariaeformis Okutani, 1990 | W Pacific | Snail Pit, Mariana Back-Arc Basin; Manus Basin | 1912–3680 | V |
|
P. pacifica Warén & Bouchet, 1986 | E Pacific | Gulf of Panama; Oregon Margin; Costa Rica Margin | 1017–2750 | F |
|
P. reticulata Warén & Bouchet, 2009 | E Atlantic | Regab, off West Africa | 3150 | S |
|
P. sculpta Warén & Ponder, 1991 | Gulf of Mexico | Off Louisiana, Gulf of Mexico | 576 | S |
|
P. segonzaci Warén & Ponder, 1991 | W Pacific | Fiji Back-Arc; Hine Hina, Lau Basin | 1750–1900 | V |
|
P. shinkaiae Okutani & Fujikura, 2002 | W Pacific | Japan Trench | 5343 | S |
|
P. stephanos |
W Pacific | Off Hatsushima, Sagami Bay | 860–908 | S |
|
P. subglabra |
W Pacific | Hatoma Knoll, Izena Hole, Irabu Knoll, Minami-Ensei Knoll, Yaeyama Knoll, Okinawa Trough; Haima Seep, South China Sea | 710–2190 | V,S |
|
P. variabilis Warén & Bouchet, 1986 | E Pacific | Endeavor Segment, Axial Seamount, Explorers Ridge, Juan de Fuca Ridge; Oregon Margin | 1500–2927 | V |
|
Costa Rica • 42 specimens; Costa Rica Margin, Jaco Scar; 9.118°N, 84.839°W; 1757 m; 20 March 2017; Elena Perez, Geoff Cook leg.; ALVIN Dive 4874, from tubeworms; SBIC M12301. 3 specimens; Costa Rica Margin, Jaco Scar; 9.115°N, 84.836°W; 1834 m; 27 March 2017; Victoria Orphan, Kat Dawson leg.; ALVIN Dive 4912, from mussels; SBIC M16110 and M16127. 1 specimen; Costa Rica Margin, Jaco Scar; 9.116°N, 84.840°W; 1898 m; 28 March 2017; Greg Rouse, Jorge Cortes leg.; ALVIN Dive 4913, from tubeworms; SBIC M16144. 10 specimens; Costa Rica Margin, Jaco Scar; 9.117°N, 84.840°W; 1802 m; 29 March 2017; Chris Roman, Alanna Durkin leg.; ALVIN Dive 4914, from tubeworms; SBIC M16153, M16164, and M16166. 7 specimens; Costa Rica Margin, Jaco Scar; 9.117°N, 84.840°W; 1806 m; 17 October 2018; Erik Cordes, Rebecca Rutstein leg.; ALVIN Dive 4971, from rocks; SBIC M16730 and M16754. 1 specimen; Costa Rica Margin, Jaco Scar; 9.118°N, 84.840°W; 1803 m; 19 October 2018; Victoria Orphan, Natalya Gallo leg.; ALVIN Dive 4973, from mussels; SBIC M16724. 1 specimen; Costa Rica Margin, Jaco Scar; 9.118°N, 84.840°W; 1803 m; 19 October 2018; Victoria Orphan, Natalya Gallo leg.; ALVIN Dive 4973, from rock; SBIC M16741. 38 specimens; Costa Rica Margin, Jaco Scar; 9.118°N, 84.840°W; 1803 m; 23 October 2018; Erik Cordes, Joanna Klein leg.; ALVIN Dive 4977, from mussels; SBIC M16807. 37 specimens; Costa Rica Margin, Jaco Scar; 9.118°N, 84.841°W; 1780 m; 4 November 2018; Erik Cordes, Melissa Betters leg.; ALVIN Dive 4989, from tubeworms. 40 specimens; Costa Rica Margin, Jaco Scar; 9.117°N, 84.840°W; 1802–1812 m; 7 January 2019; Erik Cordes, Melissa Betters leg.; SUBASTIAN Dive 214, from mussels.
Detailed in full below, the specimens of P. ios presented here were previously referred to as P. goniata (
Costa Rica • 3 specimens; Costa Rica Margin, Quepos Seep; 9.031°N, 84.619°W; 1413 m; 7 June 2017; Lisa Levin, Kris Krasnosky leg.; ALVIN Dive 4924, from mussels; SBIC M16204. 6 specimens; Costa Rica Margin, Mound 11; 8.922°N, 84.305°W; 1017 m; 3 November 2018; Victoria Orphan, Hang Yu leg.; ALVIN Dive 4988, on wood; SBIC 16955.
The range of P. pacifica is here expanded to one hydrocarbon seep (Quepos Seep) and one organic fall at the CRM (Mound 11). Their occurrence here on Bathymodiolin mussels represents the first time they have been observed as, potentially, permanent denizens of a hydrocarbon seep environment. Their distribution now includes the Oregon Margin, the Costa Rica Margin, and the Gulf of Panama between 1017–2750 m depth (Table
In total, 1,817 Provanna specimens were sampled from six sites at the CRM (see Table
Provanna morphotypes sampled from the CRM A, B P. laevis from mussel shells, Mound 12, AD4917, 965 m C, D P. ios from unknown substrate, Jaco Scar, SD214, 1803 m E Specimens of P. pacifica from sunken wood, Mound 11, AD4988, 1017 m F Specimen of P. cf. lomana from mussel shells, Quepos Seep, AD4924, 1413 m. Both the dorsal and ventral view of each shell is shown. Scale bars: 1 mm.
Across all Costa Rican specimens, measurements of shell length, shell width, aperture length, and aperture width showed significant collinearity (PCC > +0.95, all pairs). Because the whorls past the body whorl showed variable levels of degradation, shell size was represented in analyses by aperture length alone, as we had more confidence in this measurement. All species sampled were comparable in size, with Provanna ios being the largest and P. pacifica being the smallest (Fig.
A the four morphotypes sampled B–F comparison of morphological traits among each morphotype. The number of individuals represented on the graph and included in one-way ANOVAs are denoted by “n =” above or below each bar. Resultant p-values from one-way ANOVAs are denoted above each graph (p-value: 0 < *** < 0.001 < ** < 0.01 < * 0.05). Provanna cf. lomana was excluded from all ANOVAs due to the small number of individuals, but is included here for graphical comparison. Note that the graphs of Shell Roundness E and Aperture Roundness F have y-axes that do not start at zero. Scale bars: 1 mm.
CO1 sequences were obtained from our specimens of P. laevis (n = 4), P. ios (n = 2), and P. pacifica (n = 2). All efforts to amplify CO1 for specimens of P. cf. lomana were unsuccessful. CO1 sequences generated were uploaded to GenBank and assigned accession numbers (OM914402–OM914408 & OP577954). H3 sequences were obtained from our specimens of P. laevis (n = 1), P. ios (n = 2), P. pacifica (n = 2), and P. cf. lomana (n = 1). H3 sequences generated were uploaded to GenBank and assigned accession numbers (OR687645–OR687650).
Phylogenetic analyses support the inclusion of our specimens in the genus Provanna with high confidence for CO1 (Bayesian Posterior Probability (BPP) = 100, ML = 90) (Fig.
Bayesian topology of Abyssochrysoid gastropod mollusks A topology based on a 449 bp region of the mitochondrial CO1 gene. Topology was inferred using the HKY+G+I substitution model B topology based on a 266 bp region of the nuclear H3 gene. Novel sequences are bolded and highlighted in yellow. Numbers above branch nodes represent Bayesian posterior probabilities. Numbers below branch nodes represent the proportion of replicate trees in which the associated taxa clustered together in the bootstrap test (10,000 replicates). Only values above 50% are shown. The tree is drawn to scale, with branch lengths representing the number of base substitutions accumulated over time.
Bayesian phylogenetic tree of Provanna based on a 452 bp region of the mitochondrial CO1 gene. Novel sequences are bolded and highlighted in yellow. Topology was inferred using the HKY+G+I substitution model. Numbers above branch nodes represent Bayesian posterior probabilities. Numbers below branch nodes represent the proportion of replicate trees in which the associated taxa clustered together in the bootstrap test (10,000 replicates). Only values above 50 are shown. The tree is drawn to scale, with branch lengths representing the number of base substitutions accumulated over time.
Sequences of unknown identity (Provanna sp. 1 (GQ290577) and Provanna sp. 2 (GQ290578)) did not group together with any known species on the tree. Sequences from the Manus Basin that were previously identified as P. clathrata (
Average pairwise sequence divergences (APD) were computed across CO1 sequences (n = 236) (Table
Genetic distance estimates among and within known Provanna species. Distances were calculated using the Tamura 3-parameter model and 5,000 bootstrap replicates. Numbers below central margin represent the number of base substitutions per site, averaging over all sequence pairs. Numbers above central margin represents standard errors. The central margin represents within-group genetic distances. Calculations were conducted using 236 total nucleotide sequences. Outgroup = Desbruyeresia melanioides.
Provanna | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 | 15 | 16 | 17 | 18 | 19 | 20 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1. beebi | 0.00 | 0.01 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.03 |
2. cingulata | 0.06 | NA | 0.02 | 0.01 | 0.03 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.03 |
3. clathrata | 0.11 | 0.12 | 0.01 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.01 | 0.01 | 0.02 | 0.03 |
4. cooki | 0.06 | 0.06 | 0.11 | NA | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.03 |
5. exquisita | 0.09 | 0.11 | 0.08 | 0.09 | NA | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.03 | 0.03 | 0.02 | 0.02 | 0.03 | 0.02 | 0.02 | 0.02 | 0.05 |
6. fenestrata | 0.11 | 0.11 | 0.08 | 0.10 | 0.08 | NA | 0.02 | 0.02 | 0.01 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.03 |
7. glabra | 0.09 | 0.12 | 0.11 | 0.10 | 0.08 | 0.09 | 0.01 | 0.01 | 0.02 | 0.00 | 0.01 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.01 | 0.04 |
8. ios | 0.10 | 0.11 | 0.10 | 0.11 | 0.08 | 0.10 | 0.08 | 0.02 | 0.01 | 0.01 | 0.01 | 0.02 | 0.02 | 0.02 | 0.01 | 0.01 | 0.02 | 0.02 | 0.01 | 0.04 |
9. kuroshimensis | 0.10 | 0.11 | 0.11 | 0.09 | 0.10 | 0.08 | 0.08 | 0.08 | 0.01 | 0.02 | 0.01 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.02 | 0.01 | 0.03 |
10. laevis | 0.09 | 0.11 | 0.10 | 0.10 | 0.08 | 0.09 | 0.01 | 0.07 | 0.08 | 0.01 | 0.01 | 0.02 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.01 | 0.04 |
11. lomana | 0.10 | 0.10 | 0.10 | 0.08 | 0.07 | 0.08 | 0.06 | 0.08 | 0.07 | 0.07 | NA | 0.02 | 0.02 | 0.02 | 0.01 | 0.02 | 0.02 | 0.02 | 0.01 | 0.03 |
12. lucida | 0.13 | 0.12 | 0.11 | 0.11 | 0.12 | 0.12 | 0.14 | 0.13 | 0.11 | 0.14 | 0.12 | 0.00 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.03 |
13. macleani | 0.09 | 0.10 | 0.11 | 0.09 | 0.10 | 0.10 | 0.09 | 0.11 | 0.09 | 0.09 | 0.11 | 0.12 | 0.00 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.02 | 0.03 |
14. pacifica | 0.08 | 0.09 | 0.08 | 0.09 | 0.08 | 0.08 | 0.09 | 0.09 | 0.08 | 0.09 | 0.08 | 0.10 | 0.09 | 0.00 | 0.01 | 0.02 | 0.01 | 0.02 | 0.02 | 0.03 |
15. sculpta | 0.09 | 0.10 | 0.08 | 0.09 | 0.06 | 0.08 | 0.08 | 0.08 | 0.08 | 0.08 | 0.06 | 0.13 | 0.11 | 0.08 | NA | 0.02 | 0.01 | 0.02 | 0.01 | 0.03 |
16. shinkaiae | 0.09 | 0.11 | 0.10 | 0.11 | 0.10 | 0.11 | 0.09 | 0.06 | 0.09 | 0.09 | 0.09 | 0.11 | 0.11 | 0.10 | 0.09 | NA | 0.02 | 0.02 | 0.01 | 0.04 |
17. stephanos | 0.09 | 0.10 | 0.04 | 0.10 | 0.05 | 0.07 | 0.10 | 0.08 | 0.09 | 0.09 | 0.08 | 0.10 | 0.10 | 0.07 | 0.07 | 0.10 | NA | 0.01 | 0.01 | 0.03 |
18. subglabra | 0.10 | 0.10 | 0.07 | 0.11 | 0.08 | 0.09 | 0.10 | 0.10 | 0.12 | 0.10 | 0.09 | 0.14 | 0.11 | 0.12 | 0.09 | 0.11 | 0.08 | 0.01 | 0.02 | 0.03 |
19. variabilis | 0.11 | 0.11 | 0.11 | 0.11 | 0.08 | 0.10 | 0.08 | 0.04 | 0.08 | 0.08 | 0.08 | 0.13 | 0.11 | 0.10 | 0.08 | 0.07 | 0.09 | 0.11 | 0.03 | 0.03 |
20. Outgroup | 0.23 | 0.24 | 0.22 | 0.25 | 0.24 | 0.24 | 0.26 | 0.27 | 0.24 | 0.26 | 0.25 | 0.24 | 0.22 | 0.25 | 0.25 | 0.28 | 0.24 | 0.24 | 0.26 | 0.01 |
Hierarchical clustering performed by ASAP yielded 14 discreet subsets from an input of 19 hypothesized species (n = 236 sequences, p < 0.0001): (1) P. glabra-P. laevis, (2) P. variabilis-P. ios, (3) P. pacifica, (4) P. fenestrata, (5) P. cooki, (6), P. beebi, (7), P. cingulata, (8) P. exquisita-P. stephanos-P. clathrata, (9) P. sculpta, (10) P. lomana, (11) P. macleani, (12) P. subglabra, (13) P. kuroshimensis, (14) P. lucida. The threshold distance (Dt) used to partition the samples into species was 0.0496 (p < 0.0001) and the most common genetic distance between sequence pairs fell between 0.09–0.1.
1 | Only axial sculpturing | 2 |
– | Only spiral sculpturing | 3 |
– | Both axial and spiral sculpturing | 4 |
– | No sculpturing present | 5 |
2 | Axial sculpture extends to the posterior end of the aperture, but not into the basal area | P. lomana |
– | Axial sculpture does not extend to the posterior end of the aperture, instead stopping midway down the body whorl | P. chevalieri |
3 | Shell is thin and translucent; One can easily see through the shell | 6 |
– | Shell is not noticeably translucent; One cannot easily see through the shell | 7 |
4 | Sculptural elements absent | 9 |
– | Sculptural elements present | 10 |
5 | Sculptural elements present | P. beebi |
– | Sculptural elements absent | 26 |
6 | 1–3 spiral ribs on the body whorl above the posterior end of the aperture | P. lucida |
– | 4 or more spiral ribs on the body whorl above the posterior end of the aperture | P. cingulata |
7 | Central radular teeth highly diminished, being very narrow with a very truncated, cusp (see Fig. |
P. macleani |
– | Central radular teeth broad with a truncated cusp and a flat or rounded anterior ridge | P. beebi |
– | Central radular teeth broad with a very short cusp and concave anterior ridge | P. reticulata |
– | Central teeth are typical of genus with a triangular cusp | 8 |
8 | First lateral teeth have long, lobate major denticles and an obtuse buttress angle (see Fig. |
P. cooki (see Discussion) |
– | First lateral teeth have long, triangular major denticles and an acute buttress angle | P. variabilis (see Discussion) |
9 | Axial and spiral sculptures are strong, raised, and equally spaced, creating a regular lattice-like sculpture (see Fig. |
11 |
– | Regular, lattice-like sculpture is not formed | 12 |
10 | Sculptural elements are major spines (see Fig. |
13 |
– | Sculptural elements are minor spines | 14 |
– | Sculptural elements are punctuated, rounded beads | 15 |
– | Sculptural elements are blunt and sloping nodules | 16 |
11 | There are more than 30 axial ribs on the body whorl and 2–3 spiral ribs | P. admetoides |
– | There are 15–20 spiral ribs on the body whorl and 1–2 spiral ribs | P. fenestrata |
12 | Central radular teeth highly diminished and narrow with a very truncated, cusp (see Fig. |
P. macleani |
– | Central radular teeth broad with a short cusp and a flattened anterior ridge | P. chevalieri |
13 | Major spines on the second or third spiral rib on the body whorl connect at times to form a flattened shelf or keel | 17 |
– | Major spines do not obviously connect nor do they form a flattened keel | 18 |
14 | There are more than 30 axial ribs on the body whorl, forming a regular, lattice-like sculpture | P. admetoides |
– | There are fewer than 30 axial ribs on the body whorl | 19 |
15 | Shell globose; Shell roundness (Shell Width / Truncated Length) (see Fig. |
P. nassariaeformis |
– | Shell not globose; Shell roundness < 0.65 | 22 |
16 | Axial and spiral sculptures are strong, evenly raised, and equally spaced, creating a regular lattice-like sculpture (see Fig. |
P. fenestrata |
– | Axial and spiral sculptures vary in strength across the body whorl; Regular, lattice-like sculpture is not formed | 23 |
17 | Axial ribs form clear cords that are present along the entire body whorl, rectangular lattice-like sculpturing formed (see Fig. |
P. exquisita |
– | Axial ribs vary in strength along the body whorl, sometimes disappearing entirely, no clear lattice-like sculpturing formed | P. stephanos |
18 | Shell is very slender; Shell roundness (Shell Width / Truncated Length) (see Fig. |
P. shinkaiae (see Discussion) |
– | Shell roundness > 0.55 | P. ios (previously P. goniata) (see Discussion) |
19 | Central radular teeth highly diminished and narrow with a very truncated, cusp (see Fig. |
P. pacifica |
– | Central radular teeth broad with a very short, blunt cusp | P. reticulata |
– | Central radular teeth are typical of genus with a triangular cusp | 20 |
20 | Anterior end of aperture has a round, globose shape | P. muricata |
– | Anterior end of aperture has elongated, tapering shape | 21 |
21 | First lateral teeth have major denticles that are notched on the internal edge and rounded (see Fig. |
P. segonzaci |
– | First lateral teeth have major denticles that are not notched | 22 |
22 | Shell is globose; Shell roundness (Shell Width / Truncated Length) (see Fig. |
P. clathrata (see Discussion) |
– | Shell is slender; Shell roundness ≤ 0.55 | P. ios (previously goniata) (see Discussion) |
23 | Sculptural elements appear as small pockmarks and extend to the anterior end of the shell | P. beebi |
– | Sculptural elements appear as flat lines of beads arranged longitudinally, stopping abruptly at the first basal rib | P. sculpta |
24 | Axial sculpture varies in strength across the body whorl, sometimes disappearing entirely or extending only part of the way down the body whorl | P. variabilis |
– | Axial sculpture is strong and even along the body whorl | 25 |
25 | Central radular teeth are highly diminished and narrow with a very truncated, cusp (see Fig. |
P. pacifica |
– | Central radular teeth are broad with blunt cusps and rounded or flat anterior ridges | P. buccinoides |
– | Central radular teeth are typical of genus with triangular cusps | 26 |
26 | First lateral teeth have major denticles that are notched interiorly and lobate (see Fig. |
P. segonzaci |
– | Marginal teeth alternate in form between having 15–20 denticles | P. muricata |
– | Marginal teeth all have between 9–10 denticles | P. clathrata |
27 | Shell is thin and translucent, one can easily see the body through the shell | 28 |
– | Shell is not noticeably translucent | 29 |
28 | Central radular teeth have a long, triangular cusp; first lateral teeth have major denticles that are long and lobate (see Fig. |
P. annae (see Discussion) |
– | Central radular teeth have a short, triangular cusp; first lateral teeth have major denticles that are long and triangular | P. lucida (see Discussion) |
29 | Shell suture is highly constricted, giving the whorls an inflated, rounded appearance | 30 |
– | Shell suture is not highly constricted | 31 |
30 | Shell roundness (Shell Width / Truncated Length) (see Fig. |
P. abyssalis |
– | Shell roundness ~ 0.6 | P. cooki |
31 | First lateral teeth have very truncated, short denticles | P. laevis |
– | First lateral teeth have long major denticles | 32 |
32 | Central teeth have short, blunt cusps; lateral teeth have major denticles that are long, lobate (see Fig. |
P. laevis (previously P. glabra) |
– | Central teeth have long, sharp, triangular cusps; lateral teeth have major denticles that are long, lobate | P. kuroshimensis (see Discussion) |
– | Central teeth have long, sharp, triangular cusps; lateral teeth have major denticles that are long, sharp | P. subglabra (see Discussion) |
This study presents new records and gene sequences for P. laevis, P. ios, P. pacifica, and P. cf. lomana from the Costa Rica Margin. Integrating these novel morphological and genetic data, we review the distinction among species and present the first polytomous identification key for the genus Provanna. In both our morphological and genetic investigations, similarities among species were revealed and are discussed below.
Several Provanna species show little to no morphological distinction. For example, certain shell morphotypes of P. clathrata and P. ios have no discernable differences from one another besides the number of denticles on their outer marginal teeth (P. clathrata have about ten while P. ios have about 20) (Table
The smooth-shelled species P. laevis, P. glabra, P. kuroshimensis, and P. subglabra are also morphologically indistinguishable based on shell characters (Table
Specimens collected from the Costa Rica Margin revealed that not all shell characters are useful in delineating species. Despite its widespread use in taxonomic descriptions, the number of basal ribs showed notable variation within species. Furthermore, as basal ribs are often very weak and difficult to count consistently, these were not used as a taxonomically informative characters in the key, nor do we recommend their use in distinguishing species in the future.
Our genetic investigations supported most current taxonomic delimitations, finding robust genetic distances among the 19 species from which CO1 sequences exist. Nonetheless, automatic partitioning based on CO1 supported the consolidation of several species. Provanna variabilis and P. ios, for example, were not partitioned. However, as these species are distinguished in both our phylogenetic analyses as well as by their morphological characteristics, more data are needed to verify this genetic similarity before taxonomic revision is undertaken. Similarly, the species P. exquisita, P. stephanos, and P. clathrata were also not partitioned. However, as these are also distinguished in our phylogenetic analyses and by their shell and radular characteristics, we believe more data are needed to warrant collapse.
Provanna laevis from the Eastern Pacific and P. glabra from the Western Pacific exhibited significant genetic overlap in our species-level phylogeny (Fig.
Specimens of P. ios from the CRM were originally identified as P. goniata, given that their shells are decorated with major spines rather than minor spines (Fig.
Provanna are currently found in nearly every oceanic basin (Table
Finally, this study amends the biogeographic distribution of P. muricata. This species is listed as present in the North Fiji and Lau Basins in several secondary sources (
This study expands the ranges of P. laevis, P. ios, and P. pacifica to hydrocarbon seeps at the Pacific Costa Rica Margin. We also present a thorough review of the genus Provanna, consolidating the geographic distributions, genetics, and morphology for each extant species. We find that shell and radular morphological characters may be used to identify Provanna species and present the first identification key for this group. We also find that current species delineations within the genus Provanna are, for the most part, well-supported by genetic data. For those that are not, we herein synonymize P. glabra with P. laevis and P. goniata with P. ios. Future work will no doubt reveal new morphological varieties, species, and occurrences of Provanna snails. This key is designed to be a starting point from which researchers may begin this vital work.
We thank the crews of the R/V Falkor during FK19-0106, the R/V Atlantis during AT37-10, AT37-13, and AT42-03, as well as the operating teams of HOV ALVIN, ROV SUBASTIAN, and AUV Sentry from 2017–2019. We thank Ellen Strong, Greg Rouse, Charlotte Seid, Daniel Geiger, and Shannon Johnson for providing material that benefitted this project. We thank Dmitriy Dikin for his assistance in capturing scanning electron microscope images as well as Chloe Berger and Liv Nguyen for their molecular laboratory assistance. We also thank the science team aboard the R/V Thompson cruise TN401 for volunteering to test an early draft of this key. We thank Chong Chen, Eike Neubert, and one anonymous reviewer for their valuable feedback which improved this manuscript. Finally, we thank the people and nation of Costa Rica for allowing us to conduct this scientific research in their national waters.
The authors have declared that no competing interests exist.
No ethical statement was reported.
This research was supported by the National Science Foundation (OCE 1635219), Temple Uni-versity, and the American Malacological Society.
Conceptualization: EEC, MJB. Data curation: MJB. Formal analysis: MJB. Funding acquisition: EEC. Investigation: MJB. Methodology: MJB. Supervision: EEC. Validation: EEC. Visualization: MJB. Writing – original draft: MJB. Writing – review and editing: EEC.
Melissa J. Betters https://orcid.org/0000-0002-8975-257X
Erik E. Cordes https://orcid.org/0000-0002-6989-2348
Gene sequences generated in this study are accessible on GenBank under the accession numbers OM914402–OM914408, OP577954, and OR687645–OR687650. Morphological and genetic data from novel specimens are available on Github (Repository: melissajbetters/CRM_Provanna) or through correspondence with the lead author. The data underpinning the analysis reported in this paper are deposited at GBIF, the Global Biodiversity Information Facility, and are available at [https://doi.org/10.15468/4w9oc7] and [https://ipt.pensoft.net/resource?r=crm_provanna].