New species of benthopelagic copepod Xantharus (Calanoida: Scolecitrichidae) from the upper slope,eastern central New Zealand

Xantharus Andronov, 1981 is reported, for the first time from New Zealand, from the upper slope (306 m) off the southeastern coast of North Island (41°04.10′S, 176°22.05′E). Xantharus cryeri n. sp. females differ from the three known species by a combination of characters: antennules that extend to the distal border of pedigerous somite 2; ancestral segment XVIII of the antennule with 1 seta; mandible basis with 3 setae; maxilla endite 1 with 5 setae; leg 1 basis with inner distal border lined with small spinules; and leg 5 is squat, with all segments as long as wide and the 2 terminal spine‐like extensions of the terminal segment approximately as long as the articulated, inner, subterminal spine.     

New species of Spongia (Porifera: Demospongiae: Dictyoceratida) from New Zealand,and a proposed subgeneric structure

This paper is the fifth in a series revising the taxonomy of New Zealand dictyoceratid sponges (phylum Porifera, subclass Ceractinomorpha, order Dictyoceratida). Six new species of the genus Spongia are added to New Zealand's known fauna. The use of subgenera within the genus Spongia is discussed, and two new subgenera are proposed. The genus Hippospongia is revised, and an emended generic diagnosis is proposed.     

Paradigms for planktonic assemblages: 50 years of contributions from the Leigh Marine Laboratory,Northland, New Zealand

Abstract

Plankton includes the primary producers and consumers that are critical for healthy ecosystem function in the marine realm. My objective was to identify the major contributions of the Leigh Marine Laboratory to our broader understanding of planktonic assemblages. Significant contributions were made prior to 1990 on the ecology of larval fishes. From the 1990s the focus changed to the sensory biology of larval invertebrates and fishes, with a strong emphasis given to the role of reef sound in attracting potential settlers. Both early and post 1980s research has been highly influential in a paradigm shift away from passively drifting larvae that have little control over their fate. Important contributions have also been made on the dynamics of nutrient–phytoplankton interactions, larval development and aquaculture. Opportunities abound for future research on the dynamics of planktonic assemblages in shelf waters and in changing seas.     

A new species of Zelandobius (Plecoptera: Gripopterygidae: Antarctoperlinae) from the upper Rangitata River,Canterbury, New Zealand

Zelandobius edensis n. sp. is described from a spring‐fed creek in the headwaters of the Rangitata River catchment, South Canterbury, New Zealand. Adult males exhibit varying degrees of brachyptery and the only female collected also had short wings. Larvae are easily identified by their covering of long translucent hairs not found in other members of the Zelandobius confusus‐group. The link between adult and nymph was confirmed by comparing 600‐base‐pair sequences of the mitochondrial gene, cytochrome c oxidase 1. Observations suggest the life cycle may be strongly synchronised by temperature constraints on nymphal growth and development, and/or a short season suitable for feeding and reproduction by the terrestrial adults.     

西沙群岛钙扇藻属的几个新种

钙扇藻属(Udotea)植物广为分布于热带海洋，特别盛产于珊瑚礁上。绝大多数种类的分布具有很大的海区局限性，例如，一般的大西洋种类(除了个别例外)不产于印度-西太平洋海区，反过来也一样。与它们的广泛热带分布相反，对其分类研究工作做的却很少。自从1911年Gepp等对这个属进行了系统分类，报道了15种；六十几年来，只增添了一个新种和一个新变种，还没有任何藻类工作者对这属的系统分类进行研究。除Gepp等报道了它们的内部结构以外，其他藻类工作者仅简略地描述了外部形态和一些藻丝的情况。 1957年和1958年，中国科学院海洋研究所曾派调查组到我国西沙群岛进行海藻调查时，采集了113号标本。经过我们的初步分析研究，西沙群岛的钙扇藻属的区系是非常丰富的。本文所报道的六个新种，仅只是西沙群岛钙扇藻区系的一部分。所用标本，包括模式标本都保存在中国科学院海洋研究所植物标本室。     

Abergasilus amplexus Hewitt, 1978 (Ergasilidae: Copepoda) from New Zealand,with a description of the male

The male of Abergasilus amplexus Hewitt, 1978 is described for the first time. Previous records of A. amplexus are discussed and a new locality, Te Whanga Lagoon, Chatham Islands, is reported.     

Growth of red gurnard (Teleostei: Triglidae) from Pegasus bay,Canterbury, New Zealand

Growth of the red gurnard, Chelidonichthys kumu (Lesson and Garnot), from Pegasus Bay, Canterbury, was measured during 1966–67. Otoliths were used as an indicator of fish growth; mean length‐at‐age data were obtained from back‐calculated fish lengths at the time of formation of successive annual rings in the otoliths. Growth in length was found to be adequately expressed by the von Bertalanffy growth equation :

l_t = 52.0 [1 ‐ e‐^{0.406 (t‐o.291)}]

(where l_t is the fork length in cm at age t). The length: weight relationship was:

w = 78.56 × 10^‐4 l ^3.072

(where w is the weight in grams). From this relationship, growth in weight was described by the equation:

w_t = 1469 [1 ‐ e‐0.406 (t‐0.291)]³.     

Natural dispersion of mercury from Puhipuhi,northland, New Zealand

The mercury content of sediments and water in the Wairua (Wairoa) River, Northland, and of molluscs from the estuary of the river was determined to establish the extent of natural dispersion of mercury from deposits at the source of the river at Puhipuhi. The mercury content per gram wet weight of cockles, Chione stutchburyi, (0.032 ppm); rock oysters, Crassostrea glomerata, (0.081 ppm); pipi Paphies australe, (0.019 ppm); and green‐lipped mussels, Perna canaliculus, (0.017 ppm) was compared with that of specimens of the same species from other areas where presumably only background concentrations exist. Mercury could be detected in sediments at least 35 km from the deposits, but in water only up to about 8 km. Normal background levels were established for the soft parts and individual organs of the four species of mollusc investigated; of the molluscs found in the estuary of the Wairua River, only C. glomerata had anomalous amounts of mercury, but whether this indicates abnormally high mercury levels in the environment is unknown, because many other factors still need to be evaluated. Mercury levels of all molluscs were well below the generally accepted safety level of 0.5 ppm for fish for human consumption.     

Recent Ostracoda from Port Pegasus,Stewart Island,New Zealand

Sixty‐one species are listed from 19 stations in the Port Pegasus area of Stewart Island, New Zealand. A chart showing bottom sediment characteristics for all samples is included. Because of the sparseness of the sampling stations no attempt was made to evaluate ostracod distribution in terms of depth zonations or assemblages. It is hoped, however, that the information presented will aid in the interpretation of the broader provincial aspect of ostracod distribution. This paper is the first to present scanning electron micrographs to illustrate a New Zealand ostracod fauna.     

Reproductive output of male seahorses,Hippocampus abdominalis,from Wellington Harbour,New Zealand: Implications for conservation

This investigation examines aspects of reproductive output in brooding wild male seahorses, Hippocampus abdominalis, from Wellington Harbour, New Zealand. Previously undocumented, such information is crucial to the management and protection of this species in relation to the CITES Appendix II‐listing of all seahorse species. Brooding males (n = 46) were captured and kept captive until the release of their juveniles, whereupon the number of juveniles was counted and sampled for standard length (SL) and dry weight (DW). SL (mean ± 1SE) of brooding males was 18.1 ± 0.6 cm and wet weight (WW) 17.6 ± 1.6 g. Number (mean ± 1SE) of juveniles released per brood was 271.2 ± 27. The number of juveniles produced was positively correlated with parent SL, WW, and brood pouch volume. Brood pouch volume was positively correlated with male SL. SL (mean ±1SE) of juveniles released was 16.7 + 0.2 mm and DW 1.2 ± 0.1 mg. Mean SL and DW of juveniles were not correlated with the number of juveniles per brood, parent male SL or parent male pouch volume. The percentage of pouch contents which were non‐viable (i.e., premature or non‐viable eggs) upon juvenile release was low (1.1 ± 0.2%; mean ±1SE of the total pouch contents). Based on findings in this study it is suggested that the CITES 10 cm minimum height restriction, which can be used in lieu of non‐detriment findings to allow sustainable exploitation of seahorses, is not suitable for H. abdominalis from Wellington Harbour as it would appear to only protect small males that produce low numbers of juveniles.     

Biomarkers of Middle to Late Jurassic marine sediments from a canonical section: New records from the Yanshiping area,northern Tibet

The Yanshiping section, which includes the Quemo Co, Buqu, Xiali, Suowa and Xueshan Formations (Yanshiping Group) exposes organic-rich Middle to Late Jurassic deposits in the Qiangtang Basin of northern Tibet. The biostratigraphic data, from bivalves, brachiopods as well as dinoflagellate cysts, define a Bajocian to Tithonian age. This study focuses on the biomarkers present in these mudstones and limestones to determine the sources, thermal maturity and depositional environment of the organic matter. Most samples show a clear dominance of short-chain (C₁₅–C₂₀) n-alkanes with a maximum at C₁₉ or C₁₉ with a secondary maximum at C₂₃ except for the sample BP01(22)S1 where the predominant range is C₂₂ to C₂₆ with a maximum at C₂₄, significant CPI and odd-to-even predominance. The hopanoids and steroids suggest that the sources of organic matter were dominated by phytoplankton, especially algae, as the primary source. Furthermore, the Pr/Ph, Pr/nC₁₇ and Ph/nC₁₈, with relatively low values plus high abundance of 17α(H)-hopanes, support deposition in dysoxic to reducing, relatively shallow-water depositional settings, and the presence of gammacerane indicates normal marine salinity and/or water-column stratification. All samples are fairly mature with respect to petroleum generation, a conclusion supported by maturity parameters such as C₃₁ 22S/(22S + 22R) hopanes and C₂₉ ααα20S/(20S + 20R) steranes.     

First record of the crocodile shark,Pseudocarcharias kamoharai (Chondrichthyes: Lamniformes), from New Zealand waters

Commercial tuna longline fishing targeting bigeye tuna, Thunnus obesus (Lowe 1839), on the Three Kings Rise, northern New Zealand, resulted in the bycatch of a single specimen of a mature male crocodile shark, Pseudocarcharias kamoharai (Matsubara 1936). This is the first record for the New Zealand Exclusive Economic Zone, and a major southern range extension of the species in the Indo‐Pacific.     

Early oligocene squalodont cetacean from Oamaru,New Zealand

Records of Tertiary fossil cetacea from New Zealand are revised. Probable proto‐squalodontid teeth from the McDonald Limestone Formation (Whaingaroan Stage, Lower Oligocene), Oamaru, are described, and represent the oldest cetacean remains found in New Zealand. This record demonstrates the probable extension of the Squalodontidae into the Lower Oligocene.     

New Notodelphyidae (Copepoda: Cyclopoida) from New Zealand solitary ascidians

The male of Doropygus platylhorax Jones, 1974 and two new species of Doropygus (D. louisae and D. spinosus) are described and illustrated. The specimens of Doropygus described by Schellenberg (1922) as D. pulex are assigned to the new species D. louisae. Specimens of Ophioseides (Scolecimorpha) joubini described by Schellenberg (1922) have been re‐examined together with fresh material, and have been described as a new species, Ophioseides schellen‐bergi.     

Age and growth of bluenose,Hyperoglyphe antarctica (Pisces: Stromateoidei) from the lower east coast,North Island,New Zealand

Growth of the bluenose, Hyperoglyphe antarctica (Carmichael, 1818) from the lower east coast, North Island, was determined by counting growth check rings in otoliths. One growth check ring appeared to be laid down each year, so this technique is probably valid for aging bluenose. Female fish had a significantly higher growth rate than males. Comparisons of samples from three sites indicated no significant regional differences in growth. The von Bertalanffy parameters L8,K, and t0 fitted to back‐calculated fish lengths were, respectively, 81.1 cm, 0.308, ‐0.627 for males, and 86.1 cm, 0.308, ‐0.384 for females.     

Common bivalve larvae from New Zealand: Leptonacea

The late stage larvae of three erycinid bivalves (Mollusca: Pelecypoda: Leptonacea) taken from the brood chamber of the adult are described (Kellia cycladiformis, Lasaea rubra hinemoa, and L. maoria), and the provisionally identified late stage larva of the erycinid Arthritica bijurca taken from the plankton is described. Also, the D‐shaped larvae of the erycinid bivalves Kellia cycladiformis, Borniola reniformis, Arlhritica crassijormis, and A. bifurca taken from the parent brood chamber are described. The seasonal occurrence of each late stage larva in the plankton at the Bay of Islands (35° 15'S, 174° 10'E), Wellington Harbour (41° 16'S, 174° 51'E), and Raumati Beach (40° 56'S, 174° 58'E), New Zealand is described. Aspects of the reproductive cycles of Lasaea rubra hinemoa and Arthritica bifurca are presented.     

Common bivalve larvae from New Zealand: Mytilacea

The late stage larvae of five common mytilid bivalves (Mollusca: Pelecypoda: Mytilacea) are described and provisionally identified as Mytilus edulis aoteanus, Modiolus areolatus, Perna canaliculus, Xenostrobus pulex, and Modiolarca impacta. All are readily distinguishable on the basis of larval shell features, including hinge structure. However, one common species, Aulacomya maoriana, was not discerned, and thus the identifications must remain tentative.

The larvae were recovered from plankton samples from Bay of Islands (35° 15’ S, 174° 10’ E), Wellington Harbour (41° 16’ S, 174° 51’ E), and Raumati Beach (40° 56’ S, 174° 58’ E), New Zealand, during 1970–72. Their seasonal occurrences in the plankton are described and related to the condition index of the adults as far as possible.     

A new species of Boeckella (Copepoda: Calanoida) from northland,New Zealand

Boeckella tanea, n.sp. is described. It shows similarities to B. propinqua and B. delicata, and appears to be confined to lakes and ponds in Northland, New Zealand.     

Salt structures in the Laizhouwan depression, offshore Bohai Bay basin, eastern China: New insights from 3D seismic data

Using the new high-quality 3D seismic data, this paper addresses the salt structures in the KL11 area of the Laizhouwan depression in the southern offshore Bohai Bay basin. In the study area, the salt in the Sha-4 Member of the Paleogene Shahejie Formation thickened, and then formed an S–N trending salt wall, which changes shape regularly along its trend from salt diapir to salt pillow. The change in thickness of the suprasalt layers record five growth phases of the salt wall from the Eocene to the Quaternary: (1) early diapirism, (2) active diapirism, (3) passive diapirism, (4) relative structural quiescence, and (5) arching. The evolution of the salt structures was mostly governed by the multi-phase compression induced by the dextral strike-slip of the Tan–Lu fault, which formed a restraining bend in the study area. There was an original passive stock in the south, which was later tectonically squeezed by E–W compression and became a diapir. As the shortening propagated to the north from the original stock, the salt pillow was created in the north. Relative structural quiescence then followed until the next phase of compression, which arched the thick roof of the salt wall.