Occurrence and density of Halobates micans (Hemiptera: Gerridae) in the eastern South Indian Ocean

Two species of ocean skaters, Halobates germanus and Halobates micans, live in the tropical and subtropical waters of the Indian Ocean. From December 1992 to December 1993, Halobates was intensively sampled in the easternmost region of the South Indian Ocean (13–18.5°S, 114–121E°), from which there have been a small number of records of Halobates. No H. germanus was caught, but a total of 1190 H. micans were collected, with densities estimated at 13 900–28 100 individuals/km². This suggests that H. micans lives in the study area at high densities comparable to those in the Atlantic and the Pacific Oceans. We also discuss the possible effects of ocean currents and winds on the geographic distributions of the two Halobates species in the eastern South Indian Ocean.     

The sea-skater Halobates (Heteroptera: Gerridae) – probable cause for extinction in the Mediterranean and potential for re-colonisation following climate change

Sea-skaters in the genus Halobates Eschscholtz 1822 include some of the most specialised water striders and are found in tropical and subtropical seas around the world. Even though species of Halobates occur in both the Atlantic Ocean and the Red Sea, no extant sea-skater has been reported from the Mediterranean Sea. A fossil, Halobates ruffoi Andersen et al., 1994, described from Middle–Upper Eocene (45 Ma) Italy indicates that sea skaters were present in this part of the world in the past. Other geological evidence points to dramatic changes in the Mediterranean Sea during the Tertiary and Quaternary that may have led to their later extinction. In this paper we review briefly the distribution, systematics, evolution and ecology of Halobates, and discuss the potential for the Mediterranean to be recolonised following expected environmental changes due to global warming.     

The curious case of Hermodice carunculata (Annelida: Amphinomidae): evidence for genetic homogeneity throughout the Atlantic Ocean and adjacent basins

Over the last few decades, advances in molecular techniques have led to the detection of strong geographic population structure and cryptic speciation in many benthic marine taxa, even those with long‐lived pelagic larval stages. Polychaete annelids, in particular, generally show a high degree of population divergence, especially in mitochondrial genes. Rarely have molecular studies confirmed the presence of ‘cosmopolitan’ species. The amphinomid polychaete Hermodice carunculata was long considered the sole species within its genus, with a reported distribution throughout the Atlantic and adjacent basins. However, recent studies have indicated morphological differences, primarily in the number of branchial filaments, between the East and West Atlantic populations; these differences were invoked to re‐instate Hermodice nigrolineata, formerly considered a junior synonym of H. carunculata. We utilized sequence data from two mitochondrial (cytochrome c oxidase subunit I, 16S rDNA) markers and one nuclear (internal transcribed spacer) marker to examine the genetic diversity of Hermodice throughout its distribution range in the Atlantic Ocean, including the Mediterranean Sea, the Caribbean Sea, the Gulf of Mexico and the Gulf of Guinea. Our analyses revealed generally low genetic divergences among collecting localities and between the East and West Atlantic, although phylogenetic trees based on mitochondrial data indicate the presence of a private lineage in the Mediterranean Sea. A re‐evaluation of the number of branchial filaments confirmed differences between East and West Atlantic populations; however, the differences were not diagnostic and did not reflect the observed genetic population structure. Rather, we suspect that the number of branchial filaments is a function of oxygen saturation in the environment. Our results do not support the distinction between H. carunculata in the West Atlantic and H. nigrolineata in the East Atlantic. Instead, they re‐affirm the older notion that H. carunculata is a cohesive species with a broad distribution across the Atlantic Ocean.     

Biogeographical patterns of marine larval trematode parasites in two intermediate snail hosts in Europe

Aim We used published inventories of trematodes in Littorina littorea (L.) and Hydrobia ulvae (Pennant) in European seas to search for two basic biogeographical patterns in the spatial occurrence of various trematode species: (1) do parasite distribution and richness patterns in the two host snails overlap with known ecoregions of free‐living organisms; and (2) does trematode species richness in the snails follow latitudinal or longitudinal gradients? Location North East Atlantic. Methods We used multidimensional scaling (MDS), analysis of similarity (ANOSIM) and analysis of variance (ANOVA) to test whether there were overlaps of parasite distribution and richness with known ecoregions of free‐living organisms. In addition, we used linear regression analyses to test whether trematode richness in snails (corrected for sampling effort) was correlated with the latitude or longitude of the sampling sites. Results When corrected for sampling effort, mean trematode species richness per site did not differ among the different ecoregions in L. littorea. In contrast, in H. ulvae, mean species richness was much lower for sites from the Celtic Sea compared with sites from the Baltic Sea and the North Sea. Based on the results of MDS analyses, trematode species composition was distinct among ecoregions; in particular, communities from the Baltic Sea differed markedly from communities in the Celtic Sea, for both snail species. Latitude and longitude were not significantly correlated with parasite species richness in either snail species. Most trematode species had restricted distributions, and only three species in L. littorea and five species in H. ulvae occurred at more than 50% of the sites. Main conclusions There is more structure in the large‐scale distribution of trematodes in gastropods than one would expect from the large‐scale dispersal capabilities of their bird and fish final hosts. We propose mechanisms based both on limited dispersal via fish and bird final hosts and on gradients in environmental factors to explain the observed patterns.     

Genetic analysis of the populations of Japanese anchovy Engraulis japonicus from the Yellow Sea and East China Sea based on mitochondrial cytochrome b sequence

Japanese anchovy Engraulis japonicus was not only a commercial species but also a key link in the marine food chain in the Yellow Sea and East China Sea. However, in recent years, E. japonicus experienced a deep recession caused by over fishing. Therefore, determination of population genetic structure is essential to underpin resource recovery and to aid delineating and monitoring populations for fishery management. In this study, sequence variation of a 402-bp fragment of mitochondrial cytochrome b (cyt b) gene from ten populations of E. japonicus in the Yellow Sea and East China Sea was determined, detecting 73 haplotypes. Haplotype diversities and nucleotide diversities for the ten populations ranged from 0.4706 ± 0.1177 (D) to 0.9935 ± 0.210 (WH), and from 0.0014 ± 0.0013 (D) to 0.0090 ± 0.0053 (WH), respectively. Analysis of molecular variance (AMOVA) showed no significant differences at all hierarchical levels, and almost all F_ST values were non-significant, indicating no significant population genetic structure in the Yellow Sea and East China Sea. Two indistinct clades with low support values were detected and the analysis of haplotype frequency distribution showed no significant geographic differences among populations. These results supported the null hypothesis that E. japonicus within the Yellow Sea and East China Sea constituted a panmictic mtDNA gene pool. Based on the present study, the existence of separate genetic stocks in the Yellow Sea and East China Sea were not detected. Strong dispersal capacity of planktonic larvae, and ocean current could be the reasons for genetic homogeneity in this species in the Yellow Sea and East China Sea.     

The impact of Yangtze River discharge on the genetic structure of a population of the rock bream,Oplegnathus fasciatus

As a rocky reef species, Oplegnathus fasciatus displays significant geographic differences that may be congruent with patterns of molecular variation. We used 10 polymorphism microsatellite loci to characterize the genetic structure and test the impact of ocean currents and the Yangtze River on the population genetic connectivity of the rock bream, O. fasciatus, sampled from Jiaonan (JN), Zhoushan (ZS) and Taiwan (TW). The average number of alleles was 17.78, with a total of 160 alleles, and the average allele value in the East China Sea (ZS?=?13.70) was higher than that in the Yellow Sea (JN?=?6.70). The individuals at the ZS location showed the highest expected heterozygosity (He?=?0.86), Nei's genetic diversity (H?=?0.84) and Shannon genetic diversity (I?=?2.21). Genetic bottleneck tests showed that individuals had experienced a recent bottleneck effect in the JN location. AMOVA analysis showed that 12.19% of genetic variation existed among populations, indicating significant population genetic differentiation in the species. The values of the population pairwise differentiation index (F_st and Φ_pt) ranged from 0.01 to 0.29. The UPGMA tree showed two diverged genealogical branches corresponding to sampling localities (Clade A?=?JN, Clade B?=?ZS and TW) in the species. The AMOVA and STRUCTURE analyses suggested that O. fasciatus may be composed of two stocks in the examined range, and the freshwater discharge from the Yangtze River might act as a physical barrier to genetic exchange between north and south China stocks of the species.     

Phylogeography of the cold‐water barnacle Chthamalus challengeri in the north‐western Pacific: effect of past population expansion and contemporary gene flow

Aim Phylogeographical patterns of marine organisms in the north‐western Pacific are shaped by the interaction of past sea‐level fluctuations during glacial maxima and present‐day gene flow. This study examines whether observed population differentiation in the barnacle Chthamalus challengeri, which is endemic to the north‐western Pacific, can be explained by the interactions between historical glacial events and patterns of contemporary gene flow. Location Eleven locations in the north‐western Pacific. Methods Partial sequences of mitochondrial cytochrome c oxidase subunit I (COI), 12S, 16S and nuclear internal transcribed spacer 1 (ITS1) were obtained from 312 individuals. Parsimony haplotype networks and analysis of molecular variance (AMOVA) were used to determine whether the observed genetic structure corresponds to marine provinces (Kuroshio Current and China Sea Coastal Provinces), zoogeographical zones (oriental and Japan warm‐temperate zones) and/or potential refugial areas (Sea of Japan and East China Sea) in the north‐western Pacific. Neutrality tests, mismatch distribution analysis and Bayesian skyline plots were used to infer the demographic history of C. challengeri. Results In total, 312, 117, 182 and 250 sequences were obtained for COI, 12S, 16S and ITS1, respectively. A panmictic population was revealed, which did not conform to the ‘isolation by distance’ model. None of the a priori population groupings based on marine provinces, zoogeographical zones or potential refugial areas was associated with observed genetic patterns. Significant negative values from neutrality tests and the unimodal mismatch distribution and expansion patterns in Bayesian skyline plots for the COI and 16S data sets indicate a population expansion in the mid‐Pleistocene (c. 200 ka). Information from the fossil record suggests that there has been a northward range shift of this species from the East China Sea or the Palaeo‐Pacific coast of Japan to the Sea of Japan since the mid‐Pleistocene. Main conclusions Chthamalus challengeri has experienced a population expansion and range shift since the mid‐Pleistocene. The observed lack of population differentiation can be explained by this past population expansion and present‐day wide‐scale larval dispersal (owing to the long planktonic larval duration) across marine provinces, which have led to the successful establishment of the species in different zoogeographical zones and habitats.     

Wind conditions facilitate the seasonal water‐crossing behaviour of Oriental Honey‐buzzards Pernis ptilorhynchus over the East China Sea

Migratory raptors rarely fly over stretches of water larger than 25 km, although different species undertake water crossings of varying lengths, depending mainly on their wing morphology. Oriental Honey‐buzzards fly c. 680 km over the East China Sea in autumn from breeding areas in Japan to wintering areas in Southeast Asia, but avoid this long water crossing in spring. We investigated the effects of weather on this exceptional migratory behaviour and its seasonality through a maximum entropy niche modelling approach. We used data collected through satellite tracking of 31 adult birds as presence points and a set of variables related to wind, precipitation and convective condition as environmental predictors. Results of modelling showed very different, almost non‐overlapping, areas suitable for migration over the East China Sea region in autumn and spring. Suitable migration routes in autumn mostly occurred over the sea, whereas suitable areas for spring migration mostly occurred over land, suggesting that circumnavigating the East China Sea is preferable in spring. At the regional scale, wind conditions facilitate water‐crossing behaviour of Oriental Honey‐buzzards in autumn, but not in spring. Specifically, suitable tailwinds over the sea enable water‐crossing in autumn, whereas in spring, wind support and convective conditions are best over land. Our modelling did not suggest any importance of convective conditions for autumn migration. However, we expect that at smaller temporal scales, convective conditions would be a considerable facilitator of the water‐crossing behaviour in this species.     

Huia caspica gen. & comb. nov., a dinoflagellate species that recently crossed the marine‐freshwater boundary

The dinoflagellate subfamily Diplopsalidoideae encompasses 11 genera whose plate patterns show a large diversity. In a recently published molecular phylogeny (Liu et al. 2015) some of these genera (e.g. Diplopsalis, Diplopelta) are polyphyletic, suggesting that further subdivision of these genera is needed. Here we established the cyst‐theca relationship of Diplopsalis caspica by incubating cysts collected from the East China Sea. Cells of D. caspica display a plate formula of Po, X, 3′, 1a, 6″, 3c+t, ?4s, 5″′, 1″″, characterized by a small, parallelogrammic anterior intercalary plate (1a) located in the middle of the dorsal part of the epitheca. The cysts are spherical and smooth‐walled with a theropylic archeopyle. In addition, we obtained four large subunit ribosomal DNA (LSU rDNA) sequences from the germinated motile cells by single‐cell polymerase chain reaction. Strains of D. caspica from the marine environment of the East China Sea differ at 0–2 positions of LSU rDNA sequences from that of lacustrine strains from NE China. In the molecular phylogeny, D. caspica was close to Lebouraia pusilla but distant from D. lenticula, the type species of Diplopsalis. Our results support the systematic importance of plate 1a, and therefore D. caspica was transferred to a new genus, Huia. The conservative LSU rDNA sequences in H. caspica suggest that the marine‐freshwater transition occurred recently.     

First record of a rare pelagic octopod,Ocythoe tuberculata (Cephalopoda: Ocythoidae), in Korea

The family Ocythoidae is found throughout the temperate and subtropical waters of the world’s ocean and contains a single species, Ocythoe tuberculata. Recently, a single female specimen of the rare pelagic species O. tuberculata was collected off Uljin in the East Sea/Sea of Japan of Korea by squid jigging for the first time. The appearance of this species could be considered as evidence of the changes in species distribution of sea surface. However, further studies are required to investigate whether this phenomenon is temporary or continuous.     

Land masses and oceanic currents drive population structure of Heritiera littoralis,a widespread mangrove in the Indo‐West Pacific

Phylogeographic forces driving evolution of sea‐dispersed plants are often influenced by regional and species characteristics, although not yet deciphered at a large spatial scale for many taxa like the mangrove species Heritiera littoralis. This study aimed to assess geographic distribution of genetic variation of this widespread mangrove in the Indo‐West Pacific region and identify the phylogeographic factors influencing its present‐day distribution. Analysis of five chloroplast DNA fragments’ sequences from 37 populations revealed low genetic diversity at the population level and strong genetic structure of H. littoralis in this region. The estimated divergence times between the major genetic lineages indicated that glacial level changes during the Pleistocene epoch induced strong genetic differentiation across the Indian and Pacific Oceans. In comparison to the strong genetic break imposed by the Sunda Shelf toward splitting the lineages of the Indian and Pacific Oceans, the genetic differentiation between Indo‐Malesia and Australasia was not so prominent. Long‐distance dispersal ability of H. littoralis propagules helped the species to attain transoceanic distribution not only across South East Asia and Australia, but also across the Indian Ocean to East Africa. However, oceanic circulation pattern in the South China Sea was found to act as a barrier creating further intraoceanic genetic differentiation. Overall, phylogeographic analysis in this study revealed that glacial vicariance had profound influence on population differentiation in H. littoralis and caused low genetic diversity except for the refugia populations near the equator which might have persisted through glacial maxima. With increasing loss of suitable habitats due to anthropogenic activities, these findings therefore emphasize the urgent need for conservation actions for all populations throughout the distribution range of H. littoralis.     

Biochemical characteristics support the recently described species Karlodinium zhouanum (Gymnodiniales,Dinophyceae)

The small athecate dinoflagellate Karlodinium zhouanum is a species recently described in the coastal waters of China. K. zhouanum is morphologically similar to Karlodinium veneficum, a typical ichthyotoxic blooming karlotoxin‐producing species, and it is impossible to distinguish between these two species based on light microscopy. In this study, strains of K. zhouanum isolated from the East China Sea were studied. By analyzing toxins, toxicity, lipid characteristics and typical molecular and physiological traits of this species, K. zhouanum was shown to be nontoxic to brine shrimp and widely spread over the coastal waters of China. No karlotoxin‐like toxin was detected by liquid chromatography‐mass spectrometry (LC–MS). Instead of gymnodinosterol, the critical sterol in toxic K. veneficum, 27(nor)‐24S‐4α‐Methyl‐5α‐ergosta‐8(14)‐en‐3β‐ol ( NEE ) was dominant in K. zhouanum, while gymnodinosterol was absent. These sterol characteristics may provide not only support for the species separation between toxic and nontoxic species of Karlodinium but also environmental survey tools to differentiate the contribution of nontoxic Karlodinium strains, which has been unclear until now.     

The impact of Yangtze River discharge, ocean currents and historical events on the biogeographic pattern of Cellana toreuma along the China coast

Aim

Genetic data were used to measure the phylogeographic distribution of the limpet, Cellana toreuma along the China coast in order to acsertain impacts of historic events, ocean currents and especially freshwater discharge from the Yangtze River on the connectivity of intertidal species with limited larval dispersal capability.

Methodology/Principal Findings

Genetic variation in 15 populations of C. toreuma (n = 418), ranging from the Yellow Sea (YS), East China Sea (ECS) and South China Sea (SCS), were determined from partial mitochondrial cytochrome c oxidase subunit I gene. Genetic diversity and divergence based on haplotype frequencies were analyzed using CONTRIB, and AMOVA was used to examine genetic population structure. Historic demographic expansions were evaluated from both neutrality tests and mismatch distribution tests. Among the 30 haplotypes identified, a dominant haplotype No. 1 (H1) existed in all the populations, and a relatively abundant private haplotype (H2) in YS. Pairwise F_ST values between YS and the other two groups were relatively high and the percentage of variation among groups was 10.9%.

Conclusions

The high nucleotide and gene diversity in the YS, with large pairwise genetic distances and relatively high percentages of variation among groups, suggests that this group was relatively isolated from ECS and SCS. This is likely driven by historic events, ocean currents, and demographic expansion. We propose that freshwater discharge from the Yangtze River, which may act as physical barrier limiting the southward dispersal of larvae from northern populations, is especially important in determining the separation of the YS group from the rest of the Chinese populations of C. toreuma.     

Genetic divergence in lizardfishes of the genusSaurida from southern Japan

Genetic divergence in four taxa of three species ofSaurida, S. undosquamis south (S) and north (N) types,S. wanieso andS. elongata caught from the East China Sea, Sea of Hyuga and Tosa Bay, was studied based on allelic frequencies at 23 genetic loci surveyed electrophoretically. Fixed allele substitution was observed at eight loci between the S and N types ofS. undosquamis and their genetic distance was 0.5582, within a range of differentiation at the species level. The S type ofS. undosquamis was found to inhabit the Sea of Hyuga and off Cape Ashizuri along the Kuroshio Current, in addition to the East China Sea. The low level of genetic variation found for this type was discussed in relation to its restricted habitat at the edge of the continental shelf. These factors, along with some morphological characters, indicate that the two types ofS. undosquamis should be recognized as distinct species.     

Distribution and abundance of Indo‐Pacific humpback dolphins in Leizhou Bay,China

Abstract

The Indo‐Pacific humpback dolphin (Sousa chinensis) is under severe threat in Chinese waters. Only four small populations of this dolphin are known to survive in the East China Sea and South China Sea. We conducted exploratory surveys from June to September 2005, and found a population of humpback dolphins in Leizhou Bay. Thirty‐eight individuals were identified and catalogued, of which 26 were photographed and re‐identified on more than one occasion, and nine were sighted on five or more occasions each. Our preliminary estimate of the size of the Leizhou population is about 237 individuals, second only to the Pearl River estuary population. We suggest that Leizhou Bay has the potential to serve as a “humpback dolphin sanctuary” in Chinese waters.     

基于叶绿体DNA片段的槭属鸡爪槭组系统进化和生物地理学研究

东亚地区经历过复杂的地质事件及气候变化,针对东亚地区进行专科专属的植物区系及地理演化研究具有重要的意义。基于3个叶绿体片段（psbA-trnH、rpl16和trnL-trnF）,对主要分布于东亚地区的鸡爪槭组（section Palmata Pax）18个分类群的分化时间、祖先地理分布、物种扩散路径等进行了分析。叶绿体片段总长度为2,232bp,其中变异位点341个（15.2%）,有效信息位点231个（10.3%）;18个鸡爪槭组内物种（包含亚种）被高度支持为单系群（99/95/1.0）,且组内物种间的支持度相对较高;鸡爪槭组内出现物种分化的时间多集中于中新世时期,组内物种的多样性速率保持相对稳定;根据BioGeoBears分析得出,东亚大陆局部地区是该组物种的祖先分布区,且现今分布于岛屿的物种分布在不同分支。通过讨论与分析得出：我国西南地区可能是鸡爪槭组植物的起源地;东海陆桥隐没与抬升,直接影响着鸡爪槭组物种的迁移与扩散;分布于亚热带亚洲大陆的鸡爪槭组物种,存在多次往同纬度高海拔地区扩散的现象。该研究有助于对东亚地区植物生物地理历史的进一步了解。     

泉古菌醇与绿素在东海陆架区的分布及关系研究

【目的】研究东海陆架地区的沉积物中的泉古菌醇、绿素的分布及其相关关系。【方法】通过有机化学的方法将泉古菌醇和绿素从沉积物中萃取出来之后,利用高效液相色谱质谱连用对泉古菌醇进行定量检测,利用高效液相色谱对绿素进行定量检测。【结果】泉古菌醇和绿素在长江河口绝对量的分布在空间上呈现类似关系,并且受到陆源输入的影响较小。【结论】东海陆架区的泉古菌醇和绿素均为海洋产生,而非陆源输入,且两者呈现明显的相关关系,提示泉古菌醇具有指示历史时期东海表层初级生产力变化的潜在应用。     

Morphological and genetic study of Prorocentrum donghaiense Lu from the East China Sea, and comparison with some related Prorocentrum species

In this paper, the detailed morphology of Prorocentrum donghaiense Lu from both field samples and cultures was examined, and a taxonomic comparison was made between P. donghaiense and some related Prorocentrum spp. using morphological and molecular data and other published information. There were distinct differences among these species in morphological characteristics that historically have been presented as conservative features. The discrepancies extended beyond that of individual variations within the same species due to environmental factors. Therefore, these morphological features may not be conservative but, rather, polymorphic depending on environmental conditions. Based on this analysis, we suggest that the high-biomass bloom-forming species in the East China Sea, previously reported as Prorocentrum dentatum Stein, is P. donghaiense Lu. The species reported from the East China Sea and Japanese and Korean waters appear to be the same species. Molecular data also suggest that P. dentatum (CCMP1517) and P. donghaiense are genetically identical. Therefore, the geographic distribution of P. donghaiense may be much wider than expected.     

New dinoflagellate species Protoperidinium haizhouense sp. nov. (Peridiniales,Dinophyceae), its cyst‐theca relationship and phylogenetic position within the Monovela group

The number of cingular plates has been used to differentiate Protoperidinium from Peridinium and related genera. Protoperidinium is characterized by the presence of three cingular plates plus a transitional plate (3C+t). However, many Protoperidinium species have been described that exhibit different cingular plate tabulations. How these species should be classified within the genus remains unclear. To address this question, the phylogenetic relationship of four Protoperidinium species, with three or four cingular plates and lacking a transitional plate, were examined in relationship to other Protoperidinium species. These four species were germinated from cysts deposited in surface sediments collected from the East China Sea, the Bohai Sea and the Yellow Sea. Three of the isolated species, P. tricingulatum, P. americanum and P. parthenopes, were described previously. The fourth is here described as P. haizhouense sp. nov. with the plate formula Po, X, 4′, 3a, 7′′, 3C, 6S, 5′′′, 2′′′′. Differences in the cyst stages of these four species, which can be taxonomically informative, were compared. Partial large subunit ribosomal DNA sequences were obtained by single‐cell polymerase chain reaction. Maximum‐likelihood and Bayesian inference showed that these four species, P. fukuyoi and Islandinium minutum form a monophyletic clade with maximal support. The genus as a whole, however, appeared polyphyletic. Our results suggest that the presence/absence of a transitional plate is significant in the phylogeny of Protoperidinium.