Two new xylophile cytheroid ostracods (Crustacea) from Kuril-Kamchatka Trench, with remarks on the systematics and phylogeny of the family Keysercytheridae, Limno cy- theridae, and Paradoxostomatidae

Keysercythere reticulata sp. nov. and Redekea abyssalis sp. nov., collected from the wood fall submerged in the Kuril-Kamchatka Trench (Northwestern Pacific), are only the second records of the naturally occurring, wood-associated ostracod fauna from a depth of over 5000 m. At the same time, K. reticulata is the second and R. abyssalis is the third representative of their respective genera. While Keysercythere Karanovic and Brandão, 2015 species are free-living, deep-sea taxa, all Redekea de Vos, 1953 live symbiotically on the body surface of wood-boring isopods, Limnoria spp. Since R. abyssalis is the only genus representative found in the deep sea, we hypothesize that its ancestor colonized this ecosystem as a result of the symbiotic relationship. Newly collected material enabled us to update molecular phylogeny of Cythreoidea based on 18S rRNA gene sequences, especially to clarify the current systematics of the families Keysercytheridae, Limnocytheridae, and Paradoxostomatidae. The resulting phylogenetic tree supports a close relationship between Keysercythere and Redekea and a distant relationship between two Limnocytheridae lineages, Timiriaseviinae and Limnocytherinae. Consequently, we propose a transfer of Redekea from Paradoxostomatidae to Keysercytheridae, and erecting of the two limnocytherid subfamilies onto the family level. The phylogenetic analysis also implies a close relationship between the nominal Limnocytherinae genus and Keysercythere+Redekea clade, albeit with a low posterior probability, requiring further studies to clarify this.


Introduction
Wood debris is significant natural resource that provides food and habitat for various marine invertebrates whether it is washed ashore or sunk into shallow or deep seafloor (see review by Schwabe et al. 2015). Some invertebrates are highly dependent on these ephemeral habitats for their survival, e.g. the wood-boring bivalves such as genus Xylophaga Turton, 1822 (Turner 2002, Voight 2007, Bienhold et al. 2013). In addition, some animals utilize wood resources indirectly by parasitizing or living commensally on wood dwelling animals (e.g. Svavarsson 1982).
The class Ostracoda is ecologically diverse crustacean group inhabiting various aquatic environments, including wood fall. Wood-fall ostracods were first reported by de Vos (1953) who described three cytheroid ostracod species associated with the wood-boring isopod Limnoria lignorum (Rathke, 1799): Aspidoconcha limnoriae de Vos, 1953 and Redekea perpusilla de Vos, 1953 were described from the Netherlands part of the North Sea, while Laocoonella commensalis (de Vos, 1953) was described from the Caribbean Sea (Curaçao). The genus Laocoonella was proposed as the replacement name for Laocoon (see de Vos and Stock 1956), preoccupied by a parasitic mollusk genus. The three genera, Aspidoconcha de Vos, 1953, Redekea de Vos, 1953, and Laocoonella de Vos and Stock, 1956 are members to the families Keysercytheridae (Karanovic and Brandão 2015), Paradoxostomatidae (de Stock 1956, Wouters andde Grave 1992), and Cytheruridae (McKenzie 1972, Maddocks andSteineck 1987), respectively. They are rare examples of symbiotic lineages in their respective families, because most of their relatives are free-living ostracods. On the other hand, another ostracod family, Entocytheridae, consists of exclusively symbiotic species, and also contains two species, Microsyssitria nhlabane Clark, 1984 andM. indica Hart, Nair andHart, 1967, living commensally on the wood-boring isopod Sphaeroma terebrans Bate, 1866 (Hart et al. 1967;Hart and Clark 1984).
Since their first discovery, xylophile ostracods have been reported from wood fall collected from both deep and shallow seas. Maddocks and Steineck (1987) found 14 species from experimental wood panels deployed on the deep-sea floor of Atlantic, Caribbean, and Panama Basins. Among those, two genera, Thomontocypris Maddocks, 1991 and Xylocythere Maddocks and Steineck, 1987, have been reported from distant hydrothermal vent fields. Their distribution suggests faunal similarity between different types of chemosynthetic ecosystems (Van Harten 1992, Maddocks 2005, Tanaka and Yasuhara 2016. Steineck et al. (1991) review of living and fossil deep-sea, wood-associated ostracods suggested an ancient origin of xylophile ostracod fauna. Karanovic and Brandão (2015) were the first to discover a free living, deep-sea, wood-associated ostracod species from naturally sunken wood pieces. Their samples were collected from abyssal plain of the Northwestern Pacific Ocean, during the German-Russian deep-sea expedition KuramBio (Kurile Kamchatka Biodiversity Studies) (Brandt and Malyutina 2015) on board of the RV Sonne in 2012 following the footsteps of the legendary expeditions with RV Vityaz. For this new taxon (species and genus), Keysercythere enricoi Karanovic and Brandão, 2015, they erected a cytheroid family, Keysercytheridae, and also included Aspidoconcha into it. Based on a comprehensive review of the wood-fall fauna, they suggested that Keysercytheridae originated in shallow waters, and that their putative ancestor may have populated deep sea via wood fall. Karanovic and Brandão (2015) also provide for the first time a key to all living cytheroid families based on the soft parts morphology.
The superfamily Cytheroidea is by far the most diverse extant ostracod lineage found in both marine and freshwater environments, from littoral to deep-sea regions, and comprises 44 families, with majority of representatives known from the fossil record and, therefore, only after their shells (see references in Yoo et al. 2019a). Since the shell alone has a limited number of characters that tend to be homoplastic (see Karanovic et al. 2020 and references therein) there are a number of cytheroids lineages with unresolved phylogenetic position. The first insight into the phylogenetic relationship between cytheroid families based on 18S rDNA (see Yamaguchi 2003) supported homoplasticity of major taxonomic characters of the shell, such as the structure of the hinge. Karanovic and Brandão (2015) also stressed that many families need to be revised from the point of the well-established, important taxonomic characters of the soft body parts, because many lineages seem to be polyphyletic. Among others, the authors question the position of Redekea in Paradoxostomatidae, due to the morphology of its mouth parts. They also failed to include a large, mostly freshwater family, Limnocytheridae in the key, arguing that its two, currently recognized, lineages have very different morphology of important soft body parts such as maxillula and the antennula. Beside, one (Timiriaseviinae) carries eggs in the posterior extension of the shell (brood pouch) and the other (Limnocytherinae) not.
During the KuramBio II expedition (RV Sonne, 250th Expedition) (Brandt et al. 2016(Brandt et al. , 2020, we retrieved several natural wood fragments from trawled bottom sediments and found a number of ostracods, including two undescribed species -one belonging to Keysercythere and the other to Redekea. This is the second record of wood-associated ostracod fauna from abyssal plains of the world. The aim of this study is to describe the two species and update current molecular phylogeny of Cythreoidea based on 18S rRNA gene, especially to clarify the position and systematics of Keysercytheridae, Limnocytheridae, and Paradoxostomatidae. For this purpose, we sequenced the 18S rRNA region of one Keysercytheridae representative (Keysercythere enricoi), two representatives of Paradoxostomatidae (the new Redekea and R. californica de Vos and Stock, 1956), and one representative of Limnocytheridae (Gomphodella hirsuta Karanovic, 2006). Our dataset also includes 18S rRNA gene sequences of other cytheroids taxa available on GenBank.

Sampling
Wood fragments were collected from the sampling station SO250_9 at the Kuril-Kamchatka Trench region during the KuramBio II expedition (RV Sonne, 250th Expedition) on 19 August, 2016 by Agassiz-Trawl (AGT), trawled from 43° 48.43'N, 151° 44.35'E, 5134 m to 43° 47.64'N 151° 44.51'E, 5101 m. Details of the AGT deployments can be found in the KuramBio II Cruise Report (Brandt et al., 2016(Brandt et al., , 2020. The collected material was transferred to a bucket with seawater and fractionated with 500 μm and 300 μm sieves. A total of 203 ostracod specimens were picked from the remnants in the 300 μm sieve. In addition, three ostracod specimens were obtained by washing a body of Limnoria sp. The collected ostracod specimens were fixed in 96% ethanol and preserved at -20°C for taxonomic description and DNA extraction.

Morphological study
The soft body parts were separated from the valves and dissected using fine needles under a stereo-binocular microscope (SZX 12, OLYMPUS). The valves were preserved on a cardboard cell slide and the soft parts mounted in CMC-10 mounting media (Masters Company, USA), on glass slides. The specimens were then observed and sketched using a transmitted light binocular microscope (BX 51, OLYMPUS) with a differential interference contrast system and a camera lucida. The valves were platinum coated and photographed with the Hitachi S-4700 scanning electron microscope (SEM) at Eulji University (Seoul). All specimens studied herein were deposited in the Crustacea collection of the Senckenberg Research Institute and Natural History Museum Frankfurt (SMF).

DNA extraction, amplification, and sequencing
DNA was extracted from all studied specimens with lysis buffer that was prepared according to Williams et al. (1992). All polymerase chain reactions (PCR) achieved total volume of 27 μl containing: 5 μl of diluted DNA template, 1 μl of each forward and reverse primer, 15 μl ultra distilled water and 5 μl AccuPower PCR Premix (Bioneer Inc.). Fragments of nuclear 18S rDNA were amplified using the primer pairs F1/R9 and F2/R8 from Yamaguchi and Endo (2003). However, these primers were not successful for all specimens and resulted in relatively short sequences. Consequently, additional primers, described in Yu et al. (2006), were used in order to get longer sequences. The primer pair P1 and P2 was used for the initial amplification of all sequences. The PCR products from this reaction were than used as DNA templates with primer pairs P1-P1W1 and P2W1-P2 under the same PCR settings as the initial amplifications, with the exception that template was l μl or 1.5 μl and the water 17.5 μl to 18 μl. The PCR setting consisted of the initial denaturation for 5 min at 95°C. PCR setting followed by 35 cycles of 30 s denaturation at 94°C, 1 min annealing at 50°C, 1 min extension at 72°C. For all PCR amplification, a final extension was at 72°C for 10 min before decreasing to 4°C at the end. PCR products were electrophoresed with agarose 1%, 0.5X TAE buffer, and marker 100bp for 20 min at 100V to determine the presence the band size of DNA. PCR products were purified by ethanol precipitation method neutralizing by Sodium acetate pH 5.5 and sequenced in both strands to confirm sequence reliability by the Sanger method for dideoxy sequencing (Macrogen Inc., Korea).

Molecular phylogenetic analysis
All obtained sequences were visualized using Finch TV version 1.4.0 (http://www.geospiza.com/Products/finchtv. shtml) to check for the quality of signal and sites with possible low resolution, and corrected by comparing forward and reverse strands. BLAST algorithm (Altschul et al. 1990(Altschul et al. , 1997 was used to check the identity of obtained sequences. Sequences were aligned in MEGA X (Kumar et al. 2018) with ClustalW (Thompson et al. 1994) with default parameters. Beside newly obtained sequences, we also used 45 published sequences belonging to various cytheroid taxa (for the full list of GenBank numbers of the new and downloaded sequences, see Table 1). We have chosen Terrestricythere pratensis Schornikov, 1980, a member Terrestricytheroidea, the sister superfamily of Cytheroidea as the outgroup to root the tree. The ambiguous sites were removed from the alignment with the aid of GBLOCKS 0.91b (Castresana 2000). Final alignment was 1163 base pairs long and contained 207 parsimony informative sites. For the best fit evolutionary model, program jModelTest 2.1.6 (Darriba et al. 2010, Guindon andGascuel 2003) was used with the Akaike information criterion (Hurvich and Tsai 1989), which proposed GTR+I+G model of molecular evolution (Tavaré 1986). Bayesian Inference, implemented in BEAST v2.5 (Bouckaert et al. 2014), was used to estimate phylogenetic relationships. Settings included the best fit evolutionary model with four gamma categories and a strict molecular clock. Yule process (Gernhard 2008) was used as a tree prior, with BEAST default log normal distribution of the species birth rate. The analysis run for 10,000,000 generations, sampling every 1,000 generations. Software Tracer (Rambaut et al. 2018) was used to visualize results of the BEAST analyses and FigTree v1.4.3 for tree visualization.

Molecular phylogeny
Tracer analysis of the BEAST results showed that the effective sample size for all measured parameters (posterior, likelihood, priors, tree likelihood, tree height, Yule model, birth rate, etc.) was far above the recommended 200, suggesting a sound estimation of the posterior distribution. The BEAST analyses produced the phylogram presented on the Fig. 1. The monophyly of Cytheroidea has not received a high posterior probability, with low support for the Bythoceratina hanejiensis Nohara, 1987, Psammocythere oviformis Hiruta, 1991, and Uncinocythere occidentalis (Kozloff and Whitman, 1954) branches. The monophyly of the rest of the cytheroids was, on the other hand, supported with the posterior probability of 0.99. While most terminal branches received a high support (from 0.98 to 1), the deeper phylogeny was not well-resolved leading to the uncertain phylogenetic relationships between cytheroids families. Nevertheless, the most important results of this analysis are the position of the genera Gomphodella De Deckker, 1981, Limnocythere Brady, 1868, Keysercythere, and Redekea. The first two genera although members of the same family, Limnocytheridae, are far apparat on the tree, and belong to different lineages. While Gomphodella clusters (posterior probability 1) with another Timiriaseviinae genus (Metacypris Brady and Robertson, 1870), Limnocythere forms a clade with Keysercythere and Redekea. This clade received a very low support (0.67). The clade Keyesercythere-Redekea received the highest posterior probability, and, at the same time, Redekea is on the tree far from other representatives of the family Paradoxostomatidae (Chelonocytherois Tanaka and Hayashi, 2019;Paradoxo stoma Fischer, 1855, andXiphichilus Brady, 1870) to which it belongs at the moment.    Distribution. This species has been found from the abyssal plain of Northwestern Pacific, ranging from 39°43.47ʹN, 147°10.11ʹE, 5229 m to 39°42.54ʹN, 147°9.51ʹE, 5217 m (Karanovic and Brandão 2015). This study is the second record of Keysercythere enricoi, and it is collected from sunken natural wood pieces on deep-sea in the same way as previous report (Karanovic and Brandão 2015). Because we found this species approximately 600 km to the southwest from the type locality, it must be widely distributed in this area, and its distribution can be associated with natural wood falls scattered on the deep-sea floor.

Taxonomy
DNA sequence. The 18S rDNA sequence of two specimens were obtained. GenBank accession numbers are MW338924 (1704 bp) and MW338925 (1256 bp).
Keysercythere reticulata sp. nov.  Diagnosis. Shell trapezoidal in lateral view, with inflated medial portion of the shell. L around 0.38 mm. External surface of carapace reticulated characterized by polygonal muri and pitted secondary reticulation within the fossae. Sensilla long existing non-collar pores surrounded with distorted shaped sieve pores (Type C pore; see review by Danielopol et al. 2018). Hp: ejaculatory duct coiled many times; hook-like process rectangular shape with round corners and a concave along distal margin; distal lobe broad sub-triangular shape.
Description of adult male (based on holotype SMF 57053). Carapace (Figs 3, 4A-D, G) trapezoidal in lateral view, with inflated medial portion of the shell (Fig. 3). L around 0.38 mm. Greatest H situated behind middle L, equaling 35% of total L. Dorsal margin somewhat roughly rounded, dorso-anterior margin converge rapidly anteriorly to a pointed tip located near the ventral margin, ventro-anterior margin relatively gently converge comparing with dorso-anterior margin, ventral margin concave immediately situated in front of middle L. Posterior margin slightly broader than anterior margin. Both valves bearing one protrusion on posterior end. External surface reticulated characterized by polygonal muri and pitted secondary reticulation within the fossae (Fig. 4A, D, G). Sensilla long existing non-collar pores surrounded with distorted shaped sieve pores (Fig. 4G); sieve pores clearly arranged in clusters, visible as pockmarks on the inside of the shell; approximate length major axis 6-30 μm and mi- nor axis 6-12 μm (Fig. 4B, D). Some simple pores (Type A sensu Puri and Dickau, 1969) existing on rim (Fig. 4H).
Inner calcified lamella broadly developed anteriorly and posteriorly in both valves (Fig. 3). Four adductor muscle scars form a vertical row (Fig. 3). Hingement merodont: LV carrying dents in medial element, posterior element with several sockets, anterior element with several shallow sockets (Fig. 4D); RV with corresponding grooves in medial element, anterior and posterior elements elon-gated knob with shallow dents (Fig. 4B). A1 (Fig. 5A) six podomeres [four and five podomeres divided by suture, same as defined 4a and 4b by Smith and Tsukagoshi (2005) and Boxshall et al. (2010)]. First podomere bare. Second podomere 1.5 times as long as first podomere, with one lateral distal seta. Third podomere one-third as long as first podomere, with one long antero-distal seta.
Fourth to sixth podomeres same length as third podomere. Fourth podomere with one long antero-distal seta and one long lateral distal seta. Fifth podomere with three long antero-distal setae and one long postero-distal seta. Sixth podomere with two long distal setae and one long blunt tipped distal seta. A2 (Fig. 5B) five articulated podomeres. First podomere (basis) parallelogram-shaped, with setulae on antero-distal margin and one long six-annulated exopodite (spinneret seta) on antero-distal end. Second (first endopodal) podomere four-fifths as long as first podomere, with one short postero-distal spine. Third (second endopodal) podomere two-thirds as long as first podomere, with one short antero-distal seta. Fourth (third endopodal) podomere four-fifths as long as first podomere, with one stout postero-distal claw with curved tip and a row of setulae on posterior margin. Fifth (fourth endopodal) podomere small, with one stout distal claw with a row of setulae on postero-distal margin. Md (Fig. 5C, D) coxa with one dorsal seta. Coxal endite consisting of eight teeth. Palp consisting of four podomeres. First podomere (basis) with one finger-like shaped sheet (exopodite) near proximal end, one short seta on dorsal margin, two short setae on ventral margin, and four long setulous setae on ventral side of distal margin. Second podomere with one setulous ventro-distal seta, one simple and setulous dorso-distal setae. Third podomere with one stout lateral distal claw. Fourth podomere with one broad and one slender distal claws each curved distally and with a row of setae on ventral margin. Mxl (Fig. 5F) branchial plate (exopodite) with 11 plumose setae. Basal podomere with one palp (lost) and three endites. Endites: dorsal one with four simple distal setae; middle one with three simple distal setae; ventral one with three simple distal setae and one setulous distal seta. L5 (Fig. 6A) four articulated podomeres. First podomere with two plumose antero-lateral setae, one plumose antero-distal seta, and one plumose dorso-proximal seta. Second podomere half as long as first podomere, with one plumose antero-distal seta. Third podomere onethird as long as first podomere, bare. Fourth podomere half as long as first podomere, with one stout sclerotized distal claw with a few sharp spines on antero-distal margin. L6 (Fig. 6B) four articulated podomeres. First podomere with one plumose antero-lateral seta, one plumose antero-distal seta, and one plumose dorso-proximal seta.
Second podomere half as long as first podomere, with one long simple antero-distal seta. Third podomere onefourth as long as first podomere, bare. Fourth podomere three-eighths as long as first podomere, with one stout sclerotized distal claw with a few sharp spines on antero-distal margin. L7 (Fig. 6C) four articulated podomeres. First podomere with two simple antero-lateral setae and one plumose antero-distal seta. Second podomere threefourths as long as first podomere, with one plumose antero-distal seta. Third podomere one-fourth as long as first podomere with a row of setulae on distal margin. Fourth podomere half as long as first podomere, with one stout sclerotized distal claw with a few sharp spines on antero-distal margin. Brush-shaped organ absent. Hp and posterior body (Fig. 6E, F) symmetrical. Ejaculatory duct coiled many times. Hook-like process rectangular shape with round corners and a concave along distal margin. Distal lobe broad sub-triangular shape. Posterior body left and right sides bearing two setulous furcal setae. Etymology. Named after reticulated surface ornamentation of the carapace.

Distribution.
Only recorded from the type locality.

Remarks.
Keysercythere reticulata can be easily distinguished from the only other species of the genus, Keysercythere enricoi, by the carapace surface ornamentation: the former has a strongly reticulated, while the latter has smooth surface. Ventral margin of valves is concave in the new species versus convex in K. enricoi. The morphology of Hp is also different: the hook-like process is rectangular and the distal lobe is broad sub-triangular in the new species, while the hook-like process is semi-circular and the distal lobe is acute sub-triangular with sharply bended tip in K. enricoi.

Genus Redekea de Vos, 1953
Redekea abyssalis sp. nov.    central area of valves (Fig. 8A, B). Sensilla long existing non-collar pores surrounded with sieve pores (Fig. 8C): circular shaped sieve pores in anterior and posterior areas, approximate diameter 4 μm; elliptical shaped sieve pores in other areas, approximate length major axis 10-20 μm and minor axis 4-9 μm. Inner calcified lamella broadly developed in both valves (Figs 7, 8D). Four adductor muscle scars form a vertical row (Fig. 7). Hingement lophodont (Figs 7, 8D). A1 (Fig. 9A) six podomeres [four and five podomeres divided by suture, same as defined 4a and 4b by Smith and Tsukagoshi (2005) and Boxshall et al. (2010)]. First podomere bare. Second podomere three-fifths as long as first podomere with one postero-distal seta. Third podomere two-fifths as long as first podomere with one short antero-distal seta. Fourth to sixth podomeres same length as third podomere. Fourth podomere with one short antero-distal seta and one long postero-distal seta. Fifth podomere with three long antero-distal setae and one long postero-distal seta. Sixth podomere with two long distal setae and one long blunt tipped distal seta. A2 (Fig. 9B) five podomeres. First podomere (basis) parallelogram-shaped, with one long two-annulated exopodite (spinneret seta) on antero-distal end. Second (first endopodal) podomere half lengths as first podomere, with one long setulous postero-distal seta. Third and fourth podomeres fused. Third (second endopodal) podomere half lengths as first podomere, with one short antero-middle seta, one short antero-distal seta, and two short postero-distal setae. Fourth (third endopodal) podomere same length as first podomere, with one stout setulous postero-distal seta. Fifth (fourth endopodal) podomere one-fourth as long as first podomere, with one stout distal claw with a row of spines on posterior margin. Md (Fig. 9C) coxa with one slender dorsal seta. Coxal endite consisting of eight teeth. Palp consisting of three podomeres. First podomere (basis), with one short seta on ventral margin and two short dorso-distal setae. Second podomere with two short ventro-distal setae and one lateral distal seta. Third podomere, with two slender setae on ventral margin, one slender distal seta, and one stout distal claw curved distally with a row of setae on ventral margin. Mxl (Fig. 9D) branchial plate (exopodite) strong- ly reduced, consisting with 1 seta. Basal podomere with one palp (endopodite) and three endites. Palp consisting of one podomere, with three simple distal setae. Endites: dorsal one with one simple and one spatula-like distal setae; middle one with one simple and one spatula-like distal setae; ventral one with two simple distal setae. L5 (Fig. 9E) four articulated podomeres. First podomere with one antero-lateral seta, one antero-distal seta, and one dorso-lateral seta. Second podomere one-fourth as long as first podomere, with one antero-distal seta. Third podomere one-eighth as long as first podomere, bare. Fourth podomere one-fourth as long as first podomere, with one stout sclerotized distal claw with a few spines on antero-distal margin. L6 (Fig. 9F) four articulated podomeres. First podomere with one antero-lateral seta, one antero-distal seta, and one plumose dorso-lateral seta.
Second podomere half as long as first podomere, with one thick antero-distal seta. Third podomere one-sixth as long as first podomere, bare. Fourth podomere one-third as long as first podomere, with one stout sclerotized distal claw with a few spines on antero-distal margin. L7 (Fig.  9G) four articulated podomeres. First podomere with one antero-lateral spine, one antero-distal seta, and one dorso-lateral seta. Second podomere four-fifths as long as first podomere, with one thick antero-distal seta. Third podomere one-fifth as long as first podomere, bare. Fourth podomere three-fifths as long as first podomere, with one long stout sclerotized distal claw with a few spines on antero-distal margin. Brush-shaped organ absent. Oral cone (Fig. 10A) subtriangular in lateral view, with six teeth on apex and one rake-like organ with three teeth. Hp and posterior body (Fig. 10B) symmetrical. Ejaculatory duct short and curved. Hook-like process elongated conical shape. Distal lobe subtriangular. Posterior body left and right sides bearing two furcal setae.
Description of adult female (based on paratype SMF 57058). Carapace (Fig. 8E, F) sub-triangular in lateral view. LV; L 0.33 mm, H 0.20 mm: RV; L 0.33 mm, H 0.18 mm. L5 (Fig. 9H) longer than that of male in appearance. Four articulated podomeres. First podomere with two antero-lateral seta, one antero-distal seta, and one dorso-lateral seta. Second podomere four-fifths as long as first podomere, with one antero-distal seta. Third podomere two-fifths as long as first podomere, bare. Fourth podomere three-fifths as long as first podomere, with one stout sclerotized distal claw with a few spines on antero-distal margin. Copulatory organ and posterior body (Fig. 10C) female genital opening paired. Sclerotized framework of genital opening roughly circular. Genital lobe paired with each two furcal setae.
Etymology. The species epithet 'abyssalis' refers to the abyssal zone of the Pacific Ocean where the species was discovered.

Distribution.
Only recorded from the type locality.

Remarks.
To date, the genus Redekea comprised two species: the type species, R. perpusilla de Vos, 1953 andR. californica de Vos andStock, 1956. Redekea abyssalis resembles these two species in the general carapace and appendage morphology. However, there are small, but consistent differences between the new and the other two species. First of all, R. abyssalis is larger, with valve size approximately 0.3 mm, while the other two species measure approximately 0.2 mm. Secondly, R. abyssalis sp. nov. has a slender valve outline than R. perpusilla, and broader than R. californica. Thirdly, the distal claw of the male L5 in R. abyssalis has a sharply bended tip, the bending in R. perpusilla occurs at about mid-length, while in R. californica the claw is evenly curved from the proximal end all the way to its tip. Finally, distal lobe and hook-like process of Hp in R. abyssalis is shorter and narrower than that of the other two species.

Discussion
This study is only the second example of ostracods collected from the natural sunken wood in deep sea. As such, it is an important contribution to our knowledge of the natural distribution of organisms that are confined to unstable environments, such as wood pieces submerged in the deep-sea floor. According to our study, Keysercythere enricoi has a relatively wide distribution, being found 600 km from its type locality. Cytheroids do not have a planktonic larval stage and swimming ability (e.g. Rodriguez-Lazaro et al. 2012). In addition, the three species, K. enricoi, K. reticulata, and R. abyssalis have not been reported from other than wood-fall habitats in the Northwest Pacific during previous studies (Karanovic and Brandão 2015, Yoo et al. 2019b, Brandão et al. 2020. These facts indicate that the three ostracod species strongly rely on the scattered wood falls as their habitat. A wide geographical distribution of some deep-sea wood-fall fauna was explained by stepping-stone hypothesis (e.g. Romano et al. 2020). Maddocks and Steineck (1987) also noticed that ostracods used experimentally deployed wood fall as their transit points, therefore we can postulate that the three species we recorded use naturally occurring wood fall as their (only) passageways, additionally stressing out the importance of this ephemeral habitats for the life in the deep sea. Two previously known Redekea species were found on the body surface of Limnoria sp. living on the wood submerged in the shallow water, or washed up in the intertidal zone. In this study, R. abyssalis was found at more than 5,000 m, and some individuals were obtained by washing the bodies of Limnoria sp. It is likely that R. abyssalis colonized deep sea though its symbiotic relationship. A high morphological and molecular (based on the 18S rRNA) similarity between previously known and the new species suggests their close relation-ship and a common ancestor that might have lived not so long time ago in the shallow waters. Some morphological characters of Redekea abyssalis, such as a larger carapace and a reduced exopodite of the Mxl in comparison to the two shallow water species, may additionally support the hypothesis that it originated from shallow water ancestors. A similar scenario has been suggested for unrelated ostracod lineage, Bairdioidea (see Danielopol 1976).
With deeper branches having a very low support in terms of the posterior probability, results of our phylogenetic analyses do not offer meaningful solution for the interfamily relationships in the superfamily Cythreoidea. This may also be the consequence of using only one genetic marker, as it has been shown that multi-gene phylogenies provide a better signal than single-gene ones (see, for example, Gontcharov et al. 2004, Castresana 2007. The 18S rRNA marker we use has been extensively applied to infer phylogenetic relationships on different taxonomic levels, including the large-scale studies of the animal kingdom (Field et al. 1988). However, this marker cannot resolve nodes at all taxonomic levels and its efficacy varies considerably among clades, which is interpreted as an effect of rapid ancient radiation within short periods (Meyer et al. 2010). In ostracods this marker alone or in combination with other markers is also commonly used for inferring phylogenetic relationships between ostracod subclasses (Yamaguchi and Endo 2003;Tinn and Oakley 2008), families (Hiruta et al. 2016), or some of the lower systematic units (Tanaka et al. 2014;Karanovic and Sitnikova 2017). Pham et al. (2020) provided an overview of intrageneric and intrafamily distance of several genetic markers, including 18S rRNA for the entire ostracod subclass Myodocopa. They confirm that this gene varies greatly, depending on the taxon in question, but in some genera of the family Polycopidae between species distances are unusually high (see also Tanaka et al. 2014). Despite some cavities that one-gene phylogeny or incongruence between lineages in 18S phylogenetic signals may cause, our results offer a degree of clarification of the problematic systematics of some cytheroids families. This supports Karanovic and Brandão (2015) suggestions that many of those families need to be revised because several well-established and commonly used taxonomic characters display high level of interfamily variability. One example is Redekea. This genus was initially considered to be similar to the genus Cytherois Müller, 1884 (see de Vos 1953;McKenzie 1969). However, the phylogenetic position of Redekea has not been resolve, with some authors (Wouters and de Grave 1992, Tanaka and Hayashi 2019 suggesting that it belongs to Paradoxostomatidae, while others doubt this but provide no clear solution (McKenzie 1972, Karanovic andBrandão 2015). Karanovic and Brandão (2015) noted that Redekea does not have reduced mandibular palp and styliform coxa, key taxonomic characters of the Paradoxostomatidae members. The results of our analysis confirm that Redekea should be excluded from Paradoxostomatidae and placed within Keysercytheridae as this branch received the highest posterior probability support. The synapomorphies of Redekea and Keysercythere are as follows: large sieve pores or pore-clusters on carapace; sixth-segmented, slender A1; broad distal claw of mandibular palp.
Although, Limnocythere appears as a sister taxon to Keysercythere+Redekea, a low support for this branch indicates that further studies should be carried out in order to understand this relationship, if any. A potential phylogenetic signal might be a corresponding pattern of tubules associated with sieve pore canals in Keysercythere and Limnocythere (see Danielopol et al. 2018), but shell structures alone are difficult to use for resolving phylogenetic relationships since many of them seem to be homoplastic (see the Introduction). On the other hand, the tree provides an insight into the problematic systematics of Limnocytheridae, as Gomphodella and Metacypris stand far apart from Limnocythere. The first two genera are members of the well-established subfamily Timiriaseviinae (see Martens 1995, Karanovic andHumphyes 2014), and Limnocythere is the nominal genus of Limnocytherinae. The phylogenetic relationship between some Timiriaseviinae genera has been studied by several authors using cladistics methods based on morphological set of characters (Gidó et al. 2007, Savatenalinton et al. 2008, Karanovic and Humphreys 2014. Although, the resulting phylogenetic trees differ (depending on the genera included), they all basically support two living lineages: one containing genera distributed in Europe and Asia, and other having a Gondwana distribution. Recently, Danielopol et al. (2018) proposed further division of the subfamily Timiriaseviinae into three tribes: Timiriaseviini, Cytheridellini, and Gomphodellini, the last established in the same publication. Their decision was based on the presence/absence of sieve pore canals on the shell, types of other shell pores, and morphology of the A1. They failed to allocate several of the currently recognized Timiriaseviinae genera (mainly due to the lack of published information), but their results show that some of the Timiriaseviinae genera are more similar to Limnocytherinae in terms of sieve pores, than they are to each other. Sieve pores, like many other shell structures seem to be homoplastic within cytheroids lineages and often dependent on the environmental conditions , Boomer et al. 2017). Presence of a brood chamber in Timiriaseviinae was considered an important synapomorphic characters, but since this is often variable even within one genus (see Danielopol et al. 2018), this character may rather be considered a plesiomorphic one. The position of the seta on the segment of the A1 (apical in Limnocythere, lateral, or absent in Timiriaseviinae) may bare a stronger phylogenetic signal, as well as the fact that most Timiriaseviinae have a 6-segmented, while Limnocytherinae have a 5-segmented A1. However, two characters that strongly support monophyly of Timiriaseviinae and their distant relationship with Limnocytherinae are a strongly reduced maxillular palp and movable distal lobe of the hemipenis. Namely, in all Timiriaseviinae species described so far, second segment of the maxillular palp is strongly reduced while it is normally developed in Limnocytherinae. Distal lobe in Limnocytherinae is tightly fused with the main body. Limnocytherinae species in addition have simple upper ramus and elaborately developed lower ramus of the hemipenis, while the situation is opposite in Timiriaseviinae (see Martens 2003). All these morphological characters and the result of molecular phylogeny together strongly support our decision to elevate the two subfamilies, Limnocytherinae and Timiriaseviinae, onto a higher taxonomic level.