Research Article |
Corresponding author: Samuel Gómez ( samuelgomez@ola.icmyl.unam.mx ) Academic editor: Danielle Defaye
© 2017 Samuel Gómez, Karen Díaz.
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:
Gómez S, Díaz K (2017) On some new species of Ancorabolidae Sars, 1909 from the Gulf of California: the genera Ceratonotus Sars, 1909, and Dendropsyllus Conroy-Dalton, 2003 (Crustacea, Copepoda, Harpacticoida). ZooKeys 657: 43-65. https://doi.org/10.3897/zookeys.657.10725
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Two new species of two genera of the family Ancorabolidae, Ceratonotus elongatus sp. n. and Dendropsyllus californiensis sp. n., found at 1642 m and 1759 m depth, respectively, in the Southern Trough of Guaymas Basin, are described. Ceratonotus elongatus sp. n. was attributed to that genus by a series of character states of which the lack of dendroid dorsal processes on the P6-bearing somite and the presence of such processes on the first abdominal somite were definitive. This species was observed to be very close to C. thistlei Conroy-Dalton, 2003 from the San Diego Trough, and can be separated by a number of traits of which the elongated sensilla-bearing dorsal tubercles on the second abdominal somite in the new species was definitive. Dendropsyllus californiensis sp. n. has been placed within that genus given the presence of four geniculate setae on P1EXP2 and one seta on P1ENP2, one inner seta on P3EXP3, and lack of inner armature on P4EXP3. Dendropsyllus californiensis sp. n. appears to be more closely related to D. thomasi Conroy-Dalton, 2003 and D. magellanicus (George & Schminke, 1998) on account of the spinulose nature of the basis of the maxilliped, the two-segmented P4ENP, and the fused condition of the P5 baseoendopod and exopod, and seems to be even more closely related to D. thomasi by the degree of development of the lateroventral processes of the cephalothorax. Dendropsyllus californiensis sp. n. can be separated from its congeners by the relative length of the first antennulary segment, relative length of the caudal rami, and by the armature formula of P3ENP2.
Deep sea, Gulf of California, Harpacticoida , taxonomy
The macrofauna diversity of the Gulf of California is fairly well known. The Gulf is home to more than 4,916 named species of macroinvertebrates, comprising approximately 70% of the invertebrate fauna of the Gulf of California. In contrast, the open sea and the deep sea below the continental shelf are regions more poorly known (
Sediment samples for meiofaunal analyses were taken in February 2007 during the Talud X oceanographic cruise in the Southern Trough of Guaymas Basin, on board the research vessel “El Puma” of the Universidad Nacional Autónoma de México (
P1-P6 first to sixth legs;
EXP exopod;
ENP endopod;
EXP(ENP) 1(2,3) first (second, third) exopodal (endopodal) segment;
ae aesthetasc;
mya million years ago.
The type material was deposited in the Copepoda collection of the Instituto de Ciencias del Mar y Limnología, Unidad Académica Mazatlán (ICML-EMUCOP).
The map showing the sampling locations where the new species were found were prepared with GeoMapApp (http://www.geomapapp.org/) and the Global Multi-Resolution Topography (GMRT) default basemap (
Sampling sites and type localities of Ceratonotus elongatus sp. n. (circle) and Dendropsyllus californiensis sp. n. (inverted triangle). Figure prepared with GeoMapApp (http://www.geomapapp.org/) and the Global Multi-Resolution Topography (GMRT) default basemap (
One female holotype as follows: body partially dissected (leaving cephalothorax with right first antennulary segment and antenna, first thoracopod to fifth urosomite, and right P5 intact) and preserved in alcohol (ICML-EMUCOP-100207-01), left antennule and antenna, pair of mandibles, maxillules, maxillae and maxillipeds, P1-P4 and left P5, and anal somite with caudal rami dissected and mounted on four slides (ICML-EMUCOP-100207-04).
Southern Trough of Guaymas Basin, Gulf of California, México (27°01'N, 110°53'04"W), 1642 m depth (see Fig.
(based on the female only). Ancorabolidae. Cephalothorax without anterior horn-like processes, with bilateral constriction in anterior half. First half of genital double-somite without, posterior half with well-developed dendroid processes. With dorsal elongate tubercles and paired tube-pores on fourth urosomite. Caudal rami divergent, approximately 11 times as long as wide, with seven setae of which seta IV fused at base of seta V. Antennule three-segmented. Antenna with allobasis bearing one abexopodal seta; without exopod; endopod with nine setae/spines. Palp of mandible one-segmented, with five setae. Maxillule with two surface setae and seven spines on praecoxal arthrite; coxal endite with two elements; basis with six setae; exopod represented by two, endopod by three elements. Maxilla with two syncoxal endites, each with three setae; endopod represented by two setae. Maxilliped with one seta on syncoxa; endopodal claw with one accessory seta. Exopod of P1 two-segmented, of P3-P4 three-segmented. Endopod of P1-P4 two segmented; endopod of P1 as long as exopod, second endopodal segment approximately 1.7 times as long as first endopodal segment; first endopodal segment of P2 and P3 reduced, smaller than second endopodal segment; endopod of P4 much smaller than in P2 and P3, first endopodal segment twice as long as second. P5 with exopod and endopodal lobe distinct; endopodal lobe a tiny pedestal with one seta and one tube-pore; exopod elongate, slender, with three elements.
Total body length, 920 µm measured from anterior outer corner of cephalothorax to posterior margin of caudal rami; length of caudal rami, 222.5 µm (ca. 24% total body length). Body (Fig.
P2-P4-bearing somites with medial tube-pore and two posterior sensilla; dorsal dendroid processes well developed. P5-bearing somite with dorsal tube-pore, without posterior sensilla; with well-developed dorsal processes, nearly as long as in preceding somites and without backwardly directed excrescent.
Original segmentation of genital double-somite indicated by bilateral constriction; first half of genital double-somite with dorsal tube-pore, without dendroid processes, without spinular ornamentation ventrally, genital field as shown (Fig.
Caudal rami elongate, divergent, cylindrical, approximately 11 times as long as wide (Fig.
Antennule (Fig.
Antenna (Fig.
Mandible (Fig.
Maxillule (Fig.
Maxilla (Fig.
Maxilliped (Fig.
P1 (Fig.
P2-P4 (Fig.
Armature formula as follows:
P5 (Fig.
Unknown.
The specific epithet, elongatus, makes reference to the elongate dorsal tubercles on the second abdominal somite.
One female holotype as follows: body partially dissected (leaving cephalothorax, left antennule and antenna, left P1-P5, abdomen, anal somite and caudal rami intact) and preserved in alcohol (ICML-EMUCOP-100207-02), pair of mandibles, maxillules, maxillae and maxillipeds, and right P1-P5 dissected and mounted on four slides (ICML-EMUCOP-100207-03).
Southern Trough of Guaymas Basin, Gulf of California, México (26°41'06"N, 111°12'W), 1759 m depth (see Fig.
(based on the female only). Ancorabolidae. Cephalothorax with bilateral anterior constriction; with two sensilla and one tube-pore on distal corners; with paired dorsal processes anteriorly, lateroventrally, and posteriorly. Rostrum fused to cephalothorax. P2-P5-bearing somites with paired dorsal dendroid processes. Second and third urosomites fused ventrally, distinct dorsally, without dendroid processes. Caudal rami divergent, around 7.5 times as long as wide; with seven setae. Antennule three-segmented. Antenna with allobasis bearing a reduced abexopodal seta; without exopod; free endopodal segment with eight setae/spines. Mandible with one-segmented palp bearing five setae. Maxillule with two surface setae and five spines on praecoxal arthrite; coxal endite with two setae; basis with six setae; exopod represented by two, endopod by three elements. Maxilla with two syncoxal endites bearing three setae each; allobasis drawn out into strong claw, accompanied by five elements; endopod one-segmented, with two setae. Maxilliped with one seta on syncoxa; endopodal claw with one accessory seta. Exopod of P1 two-segmented, of P2-P4 three-segmented. First endopodal segment of P1 small, second segment elongate, close to 4.3 times as long as first segment, and 7.6 times as long as wide. P2 without endopod. First endopodal segment of P3 and P4 very small, second segment around 8.6 and 4.4 times as long as first segment, and 8.6 and 4 times as long as wide, respectively. P5 with baseoendopod and exopod fused; endopodal lobe a small pedestal with one naked seta and one tube-pore; exopod slender, 7.7 times as long as wide, with long subdistal tube-pore and three elements.
Total body length, 670 µm measured from anterior outer corner of cephalothorax to posterior margin of caudal rami; length of caudal rami, 145 µm (ca. 22% total body length). Body cylindrical, tapering posteriorly, without clear demarcation between prosome and urosome; integument moderately chitinised; well-developed dendroid processes as for the genus (Fig.
Second and third urosomites fused ventrally forming genital double-somite, distinct dorsally, with dorsal sensilla-bearing tubercles as shown (Fig.
Caudal rami (Fig.
Antennule (Fig.
Antenna (Fig.
Mandible (Fig.
Maxillule (Fig.
Maxilla (Fig.
Maxilliped (Fig.
P1 (Fig.
P2-P4 (Fig.
Armature formula as follows:
P5 (Fig.
Unknown.
The specific epithet, californiensis, makes reference to the Gulf of California, where the species was found.
Later,
The first species proposed herein, C. elongatus sp. n., can be undoubtedly attributed to Ceratonotus given a) the presence of dendroid processes on the posterior margin of the cephalothorax and on pedigerous somites 2-5, b) the presence of a simple conical lateroventral processes on each side of the cephalothorax, c) the presence of three geniculate setae on P1EXP2, d) the two-segmented condition of P2ENP, e) the presence of two apical setae on P2ENP2, f) the presence of two inner elements on P3EXP3, g) the discrete condition of the P5EXP, h) the insertion site of the caudal setae I and II (inserted in proximal third of caudal rami), and i) the presence of dendroid processes on the first abdominal somite (second half of the double genital-somite).
Ceratonotus elongatus sp. n. from the Guaymas Basin and C. thistlei from the San Diego Trough are similar in several respects, and a close relationship between these two species is hypothesised. The description of C. elongatus sp. n. is based on one female only, making the assessment of intraspecific variability impossible. Based on the present description, C. elongatus sp. n. and C. thistlei can be separated by the relative length of the two segments of the P2ENP (ENP2 1.6 times as long as ENP1 in C. thistlei, but ENP2 nearly 2.7 times as long as ENP1 in the new species) and P4ENP (subequal in C. thistlei, but ENP1 twice as long as ENP2 in C. elongatus sp. n.), by the armature formula of the second antennulary segment (7+(1+ae) in the new species, but 6+(1+ae) in C. thistlei), by the relative length of the caudal rami (11 times as long as wide in C. elongatus sp. n., but nine times as long as wide in C. thistlei), by the total body length (920 µm in C. elongatus sp. n., but 677 µm in C. thistlei), and above all, by the elongated sensilla-bearing dorsal tubercles on the second abdominal somite. Similar but somewhat smaller dorsal tubercles are known also for C. pectinatus, and comparatively longer tubercles have been observed for C. concavus, C. tauroides, C. vareschii, and C. steiningeri, being extremely elongated in the latter. The presence of these tubercles is not exclusive for Ceratonotus, and similar but smaller tubercles have been observed also for D. thomasi and D. magellanicus. Similar tubercles have not been observed for C. coineaui, C. thistlei, and D. antarcticus. The dorsal dendroid processes of C. elongatus sp. n. seems to be longer than in C. thistlei. However, the comparatively shorter processes of C. thistlei may be an artefact of the position of the body when observed in dorsal view, making the processes look shorter than they really are.
Ceratonotus elongatus sp. n. and C. thistlei can be separated from their congeners by a combination of several characters, i.e. the presence/absence of anterior horn-like processes of the cephalothorax (absent in C. elongatus sp. n., C. thistlei, C. coineaui and C. pectinatus, but present in C. tauroides, C. steiningeri, C. vareschii and C. concavus), the general shape and degree of development of the dorsal dendroid processes (visibly more developed in C. elongatus, C. thistlei, and C. concavus, than in the other species), the armature formula of the second and third antennulary segments of the female (the females of C. concavus and C. vareschii remain unknown; the armature formula of second segment, 7+(1+ae) in C. elongatus and C. tauroides, but 6+(1+ae) in C. pectinatus, C. thistlei, and C. steiningeri; the armature formula of third segment, 9+acrothek in C. elongatus, C. pectinatus, and C. thistlei, but 8+acrothek in C. tauroides and C. steiningeri), by the spinulose nature of the outer margin of the endopodal segment of the antenna (without spinules in C. elongatus, C. thistlei, C. coineaui, and C. pectinatus, but with dense patch of fine spinules in C. tauroides, C. steiningeri and C. vareschii), the number of elements on the first endite of the maxillary syncoxa (with two elements in C. vareschii, but with three elements in the other species), by the nature of the spinular ornamentation of the basis of the maxilliped (densely covered with fine spinules in C. vareschii and C. steiningeri, but with comparatively fewer spinules in the other species), by the general shape of their antennules and antennary segments (comparatively more elongate and slenderer in C. elongatus sp. n. and C. thistlei than in the other species), the relative length of the outer basal element of P1 (visibly longer than basis in C. elongatus sp. n., C. thistlei, C. tauroides, C. vareschii, and probably C. steiningeri, but relatively shorter in the other species), by the presence/absence of P2ENP (present in C. elongatus sp. n., C. thistlei, C. coineaui, C. pectinatus, C. concavus, C. tauroides, and C. vareschii, but absent in C. steiningeri), by the one- or two-segmented condition of P4ENP (one-segmented in C. coineaui and C. pectinatus, but two-segmented in C. elongatus sp. n., C. thistlei, C. tauroides, C. steiningeri, C. vareschii and C. concavus), by the armature formula of P4ENP (with one seta on P4ENP2 in C. elongatus sp. n., C. thistlei, C. tauroides, and C. steiningeri, with two setae on P4ENP2 in C. concavus and C. vareschii, and with one seta on the only segment of P4ENP in C. coineaui and C. pectinatus), and by the relative length of the caudal rami (11 times as long as wide in C. elongatus sp. n. and C. steiningeri, but nine and eight times as long as wide C. vareschii and C. concavus, respectively, 7.6 times as long as wide in C. thistlei, and 6.8, 6.6 and 6.5 times as long as wide in C. coineaui, C. pectinatus and C. tauroides, respectively).
The second species proposed herein, D. californiensis sp. n., has been unequivocally placed within the genus Dendropsyllus given a suite of characters defined by
The genus Dendropsyllus, when found, occurs at very low densities (for example, one single specimen of D. californiensis sp. n. was found in the present study), and most species of the genus are known from one sex only (
The formation of the Gulf of California is a very recent and complicated process that began between 130 and 90 mya during the Cretaceous when the Farallon Plate started to subduct eastward from the East Pacific Rise under the North American Plate, while the latter was moving slowly westward (
This study was financed by the Programa de Apoyo a Proyectos de Investigación e Innovación Tecnológica (PAPIIT) of the Dirección General de Asuntos del Personal Académico of the Universidad Nacional Autónoma de México (UNAM-DGAPA-PAPIIT), project IN202116 Distribución y riqueza de comunidades de microinvertebrados poco conocidos del Golfo de California, and IN217306-3 Biocenosis de invertebrados bentónicos y pelágicos en aguas profundas del Pacífico Mexicano en relación con las condiciones ambientales. Ship time was provided by the Coordinación de la Investigación Científica, UNAM. The authors thank all scientists, students and crew members for their help and support during the Talud X cruise. The authors are grateful to Dr. Ray Gerber (Saint Joseph’s College of Maine, Department of Biology) for his style and grammar review to the first draft of this manuscript, and to Dr. Kai Horst George and one anonymous referee for their constructive criticism and review of the first version of the manuscript.