Not Available

Not AvailableKoeda et al. (2014) published a review of fishes of the genus Pempheris of the Red Sea. They concluded that there are four species: P. adusta Bleeker, P. mangula Cuvier, P. nesogallica Cuvier, and a new species, P. tominagai. We show that the first three species they cite are not present in the Red Sea, as follows. (1) P. adusta is a western Pacific species (type locality Ambon), described only from the holotype, and without a dark border on the anal fin. Koeda et al. (2014) mistak-enly apply that name to P. flavicycla which is a widespread Indian Ocean species characterized by a prominent broad black border along the anal fin. Koeda et al. (2014) also redescribe P. adusta, using Indian Ocean specimens of P. flavicycla, despite the coloration difference and a 2.5% difference in the mtDNA sequence (COI) between Indian Ocean and W. Pa-cific populations. (2) P. mangula is a species from the east coast of India (type locality Visakhapatnam), clearly distinct in both gill-raker counts and a 1.1% sequence divergence in COI from its Red Sea relative P. rhomboidea. Pempheris man-gula is not found west of India, and Koeda et al. (2014) mistakenly use DNA from Oman and Madagascar to represent P. mangula, instead of genetic material available from the type locality. (3) Pempheris nesogallica (type locality Mauritius) is unknown from the Red Sea. Koeda et al. (2014) separate P. nesogallica from P. rhomboidea (their “P. mangula”) by eye size; we fail to find any difference (and they use their purported eye-size difference to erroneously rename one of the two syntypes of P. nesogallica as “P. mangula”). (4) Their new species P. tominagai is referred to as the Indian Ocean sister species of “P. schwenkii of the Pacific”; however, the type locality of P. schwenkii is the Batu Islands off the SW coast of Sumatra in the Indian Ocean. They mistakenly include specimens of a distant South African species as paratypes of P. tominagai. We have determined that P. tominagai is a valid species endemic to the Red Sea and Gulf of Aden. They mis-identify one lot of P. rhomboidea in the collection of the Hebrew University of Jerusalem as their record of P. nesogallica from the Red Sea. They misidentify the specimen in their photograph of Fig. 1B as P. adusta and use it as material for their redescription of the species, but it is now shown to be a paratype of Pempheris bexillon Mooi & Randall, 2014. Addition-ally, they regard P. malabarica Cuvier as a junior synonym of P. molucca Cuvier, but the name P. molucca is based on a fanciful painting and is unavailable as a nomen dubium. They treat Pempheris russellii Day as a junior synonym of P. man-gula; however, it is distinct in having longer pectoral fins, a larger eye, and more gill rakers. Their key to the species of Pempheris of the Red Sea is incorrect. We present a new key and conclude that only three species of Pempheris are pres-ently known from the Red Sea: P. flavicycla, P. rhomboidea, and P. tominagai.Government of Canada via the Canadian Centre for DNA Barcoding, as well as from the Ontario Genomics Institute (2008-OGI-ICI-03), Genome Canada, the Ontario Ministry of Economic Development and Innovation, and the Natural Sciences and Engineering Research Council of Canada

Population dynamics and production of the small copepod Oithona spp. in a subarctic fjord of West Greenland

13 pages, 9 figures, 1 tableThe small cyclopoid copepod Oithona is widely occurring in polar areas; however, knowledge of its biology and ecology is very limited. Here, we investigate the population dynamics, vertical distribution, and reproductive characteristics of Oithona spp. from late winter to summer, in a subarctic fjord of West Greenland. During winter-early spring, the abundance of Oithona spp. was low (1.8 × 103 ind. m-2) and the population was mainly composed of late copepodites and adults, whereas in summer, abundance peaked and younger stages dominated (1.1 × 106 ind. m-2). In general, all stages of Oithona spp. remained in the upper 100 m, with nauplii exhibiting a shallower distribution. Although no general seasonal migration was found, a deeper distribution of the adult females in winter was observed. The mean clutch size of Oithona spp. varied from 16 to 30 eggs per female, peaking in summer. Egg production rates (EPR) were low in winter-early spring (0.13 ± 0.03 eggs female-1 day-1) and reached maximum values in summer (1.6 ± 0.45 eggs female-1 day-1). EPR of Oithona spp. showed a significantly positive relationship with both temperature and protozooplankton biomass, and the development of the population seemed to be appreciably affected by temperature. Oithona spp. remained active throughout the study, stressing the key importance of these small copepods in high-latitude ecosystems, especially in periods when larger copepods are not present in the surface layer. © 2014 Springer-Verlag Berlin HeidelbergThis study was supported by the Greenland Climate Research Centre through the project 6505 to T.G. Nielsen. The research leading to these results has received funding from the European Commission FP7 EURO-BASIN (Grant Agreement: 264 933), and from the Spanish Ministry of Economy and Competitiveness through a Ph.D. fellowship (BES-2008-004231) to S. Zamora-Terol, and the project CTM2007-60052 to E. SaizPeer Reviewe

Production and fate of copepod fecal pellets across the Southern Indian Ocean

The vertical distribution of copepods, fecal pellets and the fecal pellet production of copepods were measured at seven stations across the Southern Indian Ocean from productive areas off South Africa to oligotrophic waters off Northern Australia during October/November 2006. We quantified export of copepod fecal pellet from surface waters and how much was retained. Furthermore, the potential impact of Oncaea spp. and harpacticoid copepods on fecal pellets degradation was evaluated and found to be regional substantial. The highest copepod abundance and fecal pellet production was found in the western nutrient-rich stations close to South Africa and the lowest at the central oligotrophic stations. The in situ copepod fecal pellet production varied between 1 and 1,000 μg C m−3 day−1. At all stations, the retention of fecal pellets in the upper 400 m of the water column was more than 99% and the vertical export of fecal pellets was low (<0.02 mg m−2 day−1)