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Journal articles on the topic 'Kermadec'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

O’LOUGHLIN, P. MARK, and DIDIER VANDENSPIEGEL. "Sea cucumbers collected by the Kermadec Biodiscovery Expedition 2011 (Echinodermata: Holothuroidea: Apodida and Dendrochirotida)." Zootaxa 3515, no. 1 (October 12, 2012): 60. http://dx.doi.org/10.11646/zootaxa.3515.1.4.

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Three shallow holothuroid species are recorded for the rocky shoreline of the Kermadec Islands. The new apodid speciesChiridota kermadeca sp. nov. is described. Two dendrochirotid species are reported, both previously found in New Zealand: Plesiocolochirus ignavus (Ludwig, 1875) and Pseudocnus sentus O’Loughlin & Alcock, 2000.Trois espèces peu profondes d’holothuries ont été observées sur le rivage rocheux des îles de Kermadec. Deux d’entreelles appartiennent à deux espèces de dendrochirotid également connues de Nouvelle Zélande: Plesiocolochirus ignavus(Ludwig, 1875) et Pseudocnus sentus O’Loughlin & Alcock, 2000. La troisième espèce: Chiridota kermadeca sp. nov., nouvelle pour la science, est décrite.

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2

BIRD, GRAHAM J. "Additions to the Tanaidacea (Crustacea: Peracarida) of Rangitâhua, the Kermadec Islands, from the Southwest Pacific Expedition 2017." Zootaxa 4860, no. 2 (October 12, 2020): 151–78. http://dx.doi.org/10.11646/zootaxa.4860.2.1.

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Four new species or morphospecies of tanaidaceans, all of small size (c. 1 mm), from the Rangitâhua-Kermadecs component of the Southwest Pacific Expedition 2017 survey are recorded and described: Collettea coralensis n. sp., leptocheliid sp.RK#1, Psalidichelia concinna n. g. & n. sp., and Stachyops cf. sebparri. Six had been described or recorded from the earlier Kermadec Biodiscovery Expedition 2011: Aparatanais tetradonta, Chondrochelia acrolophus, Metatanais progenitor, Paradoxapseudes floppae, Tanais sp., and Zeuxo kermadecensis. This brings the number of known tanaid species from the Rangitâhua/Kermadecs group to ten. The records of the Collettea species are notable for the shallow depths from which they were collected, 4–18 m, and the habitats sampled: coral rubble, coral encrusts on rocks, and red algae.

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3

Daughenbaugh, John. "The Recent Cypraeidae of Northern New Zealand from the Kermadec Islands to the Poor Knights Islands, Southwest Pacific Ocean (Mollusca: Gastropoda: Cypraeidae)." Festivus 50, no. 1 (February 1, 2018): 36–54. http://dx.doi.org/10.54173/f501036.

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For researchers, isolated regions at the periphery of species’ distributions hold a peculiar fascination. The causes of their remoteness vary based on: distance (e.g. the Tropical Eastern Pacific), distance and countervailing currents (e.g. the Marquesas), location in a present day gyre (e.g. the Pitcairn Group) or the absence of present day means of veliger transport (e.g. the Vema Seamount). (Daughenbaugh & Beals 2013; Daughenbaugh 2015a & b, 2017). The northern New Zealand Region from the Kermadec Islands (Kermadecs) to the coastal and shelf areas in the northernmost part of New Zealand’s North Island (Northland), including the Poor Knights Islands (PKI), constitute the distributional boundaries for a number of Cypraeidae species. The boundaries are the result of the absence of coastal shelves along the east side of the Kermadec Ridge (Ridge) and precipitous drops to abyssal depths along Northland’s east coast continental shelf. Tropical waters, with their potential to transport Cypraeidae larvae, flow eastward from southern Queensland, Australia, entrained in the Tasman Front which terminates when reaching North Cape, the northernmost tip of Northland. There, the North Cape Eddy captures most of this flow while the remainder, the East Auckland Current (EAUC), flows intermittently southward along the eastern coastal, shelf and offshore areas of Northland into waters incapable of supporting Cypraeidae populations.

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4

Sykes, W. R. "Kermadec ngaio (Myoporum, Myoporaceae)." New Zealand Journal of Botany 25, no. 4 (October 1987): 595–601. http://dx.doi.org/10.1080/0028825x.1987.10410090.

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5

McCormack, Fiona. "The Kermadec Ocean Sanctuary: Terraqueous Territorialization and Māori Marine Environments." Pacific Affairs 94, no. 1 (March 1, 2021): 77–96. http://dx.doi.org/10.5509/202194177.

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This paper interprets the disrupted establishment of the Kermadec Ocean Sanctuary, a 620,000 square kilometre marine protection area, as a crucial moment in Pacific frontier making. The development of large-scale protected marine areas is a politically charged frontier tool, in which states garner international recognition and environmental renown by setting aside large swathes of their exclusive economic zones. In the Kermadec Sanctuary, this enclosure hit against an assemblage of Indigenous histories, ecologies, repatriated fishing rights, and privatized fishing quota challenging the oftmarginalized agency of Indigenous people in frontier narratives. This paper argues that three factors are fundamental to untangling this conflict: first, the historical trajectory of terraqueous territorialization in the Kermadec region, second, the post-Treaty of Waitangi settlement dynamics of Maori marine environments, and third, the common ecosystem services model underlying conservation and extraction.

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6

JUST, JEAN. "Remarkable Australasian marine diversity: 18 new species in Pentaceration Just, 2009 (Crustacea, Isopoda, Paramunnidae)." Zootaxa 2813, no. 1 (April 8, 2011): 1. http://dx.doi.org/10.11646/zootaxa.2813.1.1.

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Eighteen new species in Pentaceration Just, 2009 (Isopoda, Paramunnidae) are described. From the Arafura Sea: Pentaceration bifida; from south eastern Australia: P. bovicornis, P. denticornis, P. globopleonis, P. lancifera, P. magna, P. megalomos, P. omalos, P. rihothalassa, P. serrata, P. simplex, P. tasmaniensis; from New Zealand: P. curvicornis, P. dentifera, P. novaezealandia, P. epipedos, P. setosa; from the Kermadec Trench: P. kermadecia. A key to the 20 known species of Pentaceration is given. Pentaceration is the most diverse genus in the Paramunnidae and has the greatest depth range (7 to 5340 meters). The general distribution of the genus and the presence of species with functional eyes at shelf depth (all other species blind) suggest a shallow water Gondwana origin.

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7

HOESE, DOUGLASS F., and ANDREW L. STEWART. "A new species of the gobiid genus Eviota (Teleostei: Gobioidei) from the Kermadec Islands, New Zealand." Zootaxa 3418, no. 1 (August 10, 2012): 61. http://dx.doi.org/10.11646/zootaxa.3418.1.5.

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Eviota kermadecensis is described as a new species from the Kermadec Islands, mainly from Raoul Island, and is the onlyspecies of Eviota known from the Kermadec Islands. It is most similar to E. abax and E. masudai from Japan in morphol-ogy and fin-ray counts. All three species normally have I,10 second dorsal fin-ray counts. Eviota kermadecensis differs largely in coloration. The species has a ratio of 1.5 females to males and males average a larger size.

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8

NG, PETER K. L., and COLIN L. MCLAY. "Two new species of deep-water xanthid crabs of the genera Euryxanthops Garth & Kim, 1983, and Medaeops Guinot, 1967 (Crustacea: Decapoda: Brachyura: Xanthidae) from New Zealand." Zootaxa 1505, no. 1 (June 14, 2007): 37–50. http://dx.doi.org/10.11646/zootaxa.1505.1.3.

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Two new species of deep-water xanthid crabs, Euryxanthops chiltoni, new species, and Medaeops serenei, new species, are described from the Kermadec Islands, New Zealand. This is the first time these genera are reported from New Zealand. Keys for the identification of all species of Euryxanthops and Medaeops are provided. The two new species bring the total number of species of xanthids from the Kermadec Is. to 17, and the known species of Euryxanthops and Medaeops to five and six respectively;. Although caught in the vicinity of hydrothermal vents, there is no evidence that these species are directly dependent upon the vent community.

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9

AHYONG, SHANE T. "First records of Thryaplax Castro, 2007 and Calocarcinus Calman, 1909 (Crustacea: Decapoda: Brachyura) from the Kermadec Islands, New Zealand." Zootaxa 1982, no. 1 (January 19, 2009): 66–68. http://dx.doi.org/10.11646/zootaxa.1982.1.4.

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Among the Brachyura from the Kermadec Islands in the invertebrate collection of the National Institute of Water and Atmospheric Research, Wellington, New Zealand (NIWA), are two specimens representing two deep-water species previously not known from the region. Both specimens were collected at the same station, together with the paratypes of the parthenopid crab, Garthambrus tani Ahyong, 2008. The new records are reported below to formally document their occurrence at the Kermadec Islands, New Zealand; both also represent the first records of their respective genera from New Zealand waters. Measurements of specimens, in millimetres, refer to carapace length (cl) and carapace width (cw).

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10

Francis, Malcolm P., Roger V. Grace, and Chris D. Paulin. "Coastal fishes of the Kermadec Islands." New Zealand Journal of Marine and Freshwater Research 21, no. 1 (March 1987): 1–13. http://dx.doi.org/10.1080/00288330.1987.9516194.

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11

Chiswell, Stephen M., and Mike I. Moore. "Internal Tides near the Kermadec Ridge." Journal of Physical Oceanography 29, no. 5 (May 1999): 1019–35. http://dx.doi.org/10.1175/1520-0485(1999)029<1019:itntkr>2.0.co;2.

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12

Kosmynin, Vladimir N. "Shallow-water Scleractinian corals from Kermadec Islands." Atoll Research Bulletin 418 (1994): 1–5. http://dx.doi.org/10.5479/si.00775630.418.1.

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13

Sasakawa, Mitsuhiro. "Agromyzidae (Diptera) from Kermadec Islands, New Zealand." New Zealand Entomologist 33, no. 1 (February 2010): 14–16. http://dx.doi.org/10.1080/00779962.2010.9722186.

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14

Blum, Joel D., Jeffrey C. Drazen, Marcus W. Johnson, Brian N. Popp, Laura C. Motta, and Alan J. Jamieson. "Mercury isotopes identify near-surface marine mercury in deep-sea trench biota." Proceedings of the National Academy of Sciences 117, no. 47 (November 16, 2020): 29292–98. http://dx.doi.org/10.1073/pnas.2012773117.

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Mercury isotopic compositions of amphipods and snailfish from deep-sea trenches reveal information on the sources and transformations of mercury in the deep oceans. Evidence for methyl-mercury subjected to photochemical degradation in the photic zone is provided by odd-mass independent isotope values (Δ199Hg) in amphipods from the Kermadec Trench, which average 1.57‰ (±0.14,n= 12, SD), and amphipods from the Mariana Trench, which average 1.49‰ (±0.28,n= 13). These values are close to the average value of 1.48‰ (±0.34,n= 10) for methyl-mercury in fish that feed at ∼500-m depth in the central Pacific Ocean. Evidence for variable contributions of mercury from rainfall is provided by even-mass independent isotope values (Δ200Hg) in amphipods that average 0.03‰ (±0.02,n= 12) for the Kermadec and 0.07‰ (±0.01,n= 13) for the Mariana Trench compared to the rainfall average of 0.13 (±0.05,n= 8) in the central Pacific. Mass-dependent isotope values (δ202Hg) are elevated in amphipods from the Kermadec Trench (0.91 ±0.22‰,n= 12) compared to the Mariana Trench (0.26 ±0.23‰,n= 13), suggesting a higher level of microbial demethylation of the methyl-mercury pool before incorporation into the base of the foodweb. Our study suggests that mercury in the marine foodweb at ∼500 m, which is predominantly anthropogenic, is transported to deep-sea trenches primarily in carrion, and then incorporated into hadal (6,000-11,000-m) food webs. Anthropogenic Hg added to the surface ocean is, therefore, expected to be rapidly transported to the deepest reaches of the oceans.

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15

LEDUC, DANIEL, and ZENG QI ZHAO. "Molecular characterization of free-living nematodes from Kermadec Trench (Nematoda: Aegialoalaimidae, Xyalidae) with description of Aegialoalaimus tereticauda n. sp." Zootaxa 4949, no. 2 (March 25, 2021): 341–52. http://dx.doi.org/10.11646/zootaxa.4949.2.7.

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The Kermadec Trench is the world’s fifth deepest trench and extends from approximately 26 to 36°S near the northeastern tip of New Zealand’s North Island. Here, we describe a new species of Aegialoalaimus, a nematode genus with unusual buccal cavity and pharynx morphology, from a site at 9540 metres water depth in Kermadec Trench, and provide the first SSU and D2–D3 of LSU sequences for Aegialoalaimus, Manganonema, Metasphaerolaimus constrictus and Daptonema amphorum. Aegialoalaimus tereticauda n. sp. is characterised by body length 755–864 µm, cephalic sensilla papilliform (< 1 µm long), excretory pore located slightly anterior to posterior bulb in males and slightly anterior to nerve ring in females, arcuate spicules 18–22 µm long, gubernaculum present, precloacal supplements absent, and cylindrical tail 58–64 µm long with rounded tip. Relationships between Aegialoalaimus and Chromadorean orders could not be elucidated based on our SSU analysis; no link could be found with the Plectida, where the Aegialoalaimidae is currently placed, or with the Isolamiida or Cylindrolaimus (Areaolaimida), which share a similar and unusual buccal and pharynx morphology. Our SSU phylogenetic analysis confirms the placement of Manganonema within the Xyalidae, although relationships with other xyalid genera remain unclear. The Sphaerolaimidae formed a clade together with the Monhysteridae, which contradicts the current classification where the Sphaerolaimidae and Xyalidae are classified together into the superfamily Sphaerolaimoidea and the Monhysteridae into the Monhysteroidea. Although limited research has been conducted on the nematode diversity in Kermadec Trench to date, the available data show that half of all invertebrate species known from the trench are nematodes, which highlights the importance of conducting further taxonomic research on this group in hadal environments.

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16

Leduc, Daniel. "New free-living nematode species and records (Chromadorea: Plectida and Desmodorida) from the edge and axis of Kermadec Trench, Southwest Pacific Ocean." PeerJ 9 (September 24, 2021): e12037. http://dx.doi.org/10.7717/peerj.12037.

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One new nematode species is described and two new species records are provided from the edge (6,080 m depth) and axis (7,132 m) of Kermadec Trench, Southwest Pacific. Leptolaimus hadalis sp. nov. is characterised by medium body 587–741 μm long, labial region not offset from body contour, inconspicuous labial sensilla, amphid located 12–19 μm from anterior end, female without supplements, male with four tubular precloacal supplements (alveolar supplements absent), tubular supplements almost straight with dentate tip, arcuate spicules and weakly cuticularized dorsal gubernacular apophyses strongly bent distally. In a previously published ecological survey of Kermadec Trench, L. hadalis sp. nov. was the most abundant species in a core obtained at 8,079 m water depth and third most abundant species in a core obtained at 7,132 m, while only one individual was found at 6,096 m depth, and none at 9,175 m depth (Leduc & Rowden, 2018). Alaimella aff. cincta and Desmodora aff. pilosa are recorded for the first time from the Southwest Pacific region. Prior to the present study, Alaimella had only been recorded from coastal locations and from the Weddell sea to a depth of 2,000 m. The record of Desmodora aff. pilosa at 6,080 m depth is the deepest record of a Desmodora species to date, although unidentified Desmodora specimens have been found as deep as 6,300 m in the South Sandwich Trench. The morphology of the Kermadec Trench Alaimella aff. cincta and Desmodora aff. pilosa specimens bear a strong resemblance to their respective type populations from the Northern Hemisphere, but further morphological and molecular data are required to ascertain whether they in fact represent distinct species.

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17

Kim, JJH, L. Liggins, and JD Aguirre. "Social environment mediates habitat shifts in a range-restricted giant limpet." Marine Ecology Progress Series 666 (May 20, 2021): 89–98. http://dx.doi.org/10.3354/meps13667.

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The individuals of many species shift habitats at different stages in their lives. Sometimes, these habitat shifts coincide with an ontogenetic transition. These ontogenetic habitat shifts can allow species to access nutritional resources, avoid conspecific aggression or predation, or secure breeding opportunities when it is advantageous to do so. The Kermadec Islands giant limpet Scutellastra kermadecensis is a protandrous hermaphrodite endemic to Rangitāhua, the Kermadec Islands. These limpets have an unusual habit whereby small limpets (piggies) piggy-back on the shells of larger individuals rather than living on the rocky substrate. We investigated whether the ontogenetic habitat shift between the piggy-backing and rock-attached limpets was determined by the availability of free space on the rock or whether the ontogenetic habitat shift was a response to the properties of the surrounding limpet population. We found that the available rock space did not influence the size at which an individual transitioned from being a piggy to being rock-attached. Furthermore, larger rock-attached limpets were more likely to have piggies, they had more piggies, and the piggies were larger. Overall, our results suggest that Kermadec giant limpets are motivated to piggy-back by the properties of the social environment rather than space constraints. The piggy-backing behaviour may be a mechanism to avoid bulldozing by larger limpets, to access grazing opportunities on the shells of larger limpets, and/or to monopolise breeding opportunities with larger rock-attached females. We discuss the repercussions of this life-history strategy for this extremely range-restricted species, with reference to how these populations may be monitored and maintained.

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18

IREDALE, TOM. "The Surface Breeding Petrels of the Kermadec Group." Ibis 56, no. 3 (April 3, 2008): 423–36. http://dx.doi.org/10.1111/j.1474-919x.1914.tb04081.x.

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19

Billen, Magali I., Michael Gurnis, and Mark Simons. "Multiscale dynamics of the Tonga-Kermadec subduction zone." Geophysical Journal International 153, no. 2 (May 2003): 359–88. http://dx.doi.org/10.1046/j.1365-246x.2003.01915.x.

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20

Beever, Jessica E., Allan J. Fife, and Carol J. West. "Mosses of the Kermadec Islands, northern New Zealand." New Zealand Journal of Botany 34, no. 4 (December 1996): 463–71. http://dx.doi.org/10.1080/0028825x.1996.10410127.

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21

Eikenaar, Cas, and Adrian Skerrett. "First record of Kermadec Petrel Pterodroma neglecta for Seychelles." Bulletin of the African Bird Club 13, no. 1 (March 2006): 88–90. http://dx.doi.org/10.5962/p.309776.

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22

Baker, E. T., S. L. Walker, R. W. Embley, and C. E. J. De ronde. "High-Resolution Hydrothermal Mapping of Brothers Caldera, Kermadec Arc." Economic Geology 107, no. 8 (November 23, 2012): 1583–93. http://dx.doi.org/10.2113/econgeo.107.8.1583.

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23

Harrow, Susan. "Francis Ponge et Eugène de Kermadec: Histoire d'un Compagnonnage." Modern & Contemporary France 21, no. 2 (May 2013): 255–56. http://dx.doi.org/10.1080/09639489.2012.753427.

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24

Lloyd, E. F., Simon Nathan, I. E. M. Smith, and R. B. Stewart. "Volcanic history of Macauley Island, Kermadec Ridge, New Zealand." New Zealand Journal of Geology and Geophysics 39, no. 2 (June 1996): 295–308. http://dx.doi.org/10.1080/00288306.1996.9514713.

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25

Sutherland, R., J. Collot, F. Bache, S. Henrys, D. Barker, G. H. Browne, M. J. F. Lawrence, et al. "Widespread compression associated with Eocene Tonga-Kermadec subduction initiation." Geology 45, no. 4 (February 7, 2017): 355–58. http://dx.doi.org/10.1130/g38617.1.

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26

Hochman, Hugh. "Francis Ponge et Eugène de Kermadec, histoire d’un compagnonnage." Romanic Review 104, no. 1-2 (January 1, 2013): 177–79. http://dx.doi.org/10.1215/26885220-104.1-2.177.

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27

Sykes, W. R. "Scaevola gracilis(Goodeniaceae) in the Kermadec Islands and Tonga." New Zealand Journal of Botany 36, no. 4 (December 1998): 671–73. http://dx.doi.org/10.1080/0028825x.1998.9512604.

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28

Jordan, S. "Francis Ponge et Eugene de Kermadec: histoire d'un compagnonnage." French Studies 67, no. 1 (December 21, 2012): 119. http://dx.doi.org/10.1093/fs/kns278.

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29

Luo, Qing, and Guoliang Zhang. "Control of subduction rate on Tonga-Kermadec arc magmatism." Journal of Oceanology and Limnology 36, no. 3 (May 2018): 687–99. http://dx.doi.org/10.1007/s00343-018-7026-8.

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30

Higham, Thomas, and Leigh Johnson. "The prehistoric chronology of Raoul Island, the Kermadec Group." Archaeology in Oceania 32, no. 3 (October 1997): 207–13. http://dx.doi.org/10.1002/j.1834-4453.1997.tb00389.x.

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31

Owen, Clare, Luke Rendell, Rochelle Constantine, Michael J. Noad, Jenny Allen, Olive Andrews, Claire Garrigue, et al. "Migratory convergence facilitates cultural transmission of humpback whale song." Royal Society Open Science 6, no. 9 (September 4, 2019): 190337. http://dx.doi.org/10.1098/rsos.190337.

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Cultural transmission of behaviour is important in a wide variety of vertebrate taxa from birds to humans. Vocal traditions and vocal learning provide a strong foundation for studying culture and its transmission in both humans and cetaceans. Male humpback whales ( Megaptera novaeangliae ) perform complex, culturally transmitted song displays that can change both evolutionarily (through accumulations of small changes) or revolutionarily (where a population rapidly adopts a novel song). The degree of coordination and conformity underlying song revolutions makes their study of particular interest. Acoustic contact on migratory routes may provide a mechanism for cultural revolutions of song, yet these areas of contact remain uncertain. Here, we compared songs recorded from the Kermadec Islands, a recently discovered migratory stopover, to multiple South Pacific wintering grounds. Similarities in song themes from the Kermadec Islands and multiple wintering locations (from New Caledonia across to the Cook Islands) suggest a location allowing cultural transmission of song eastward across the South Pacific, active song learning (hybrid songs) and the potential for cultural convergence after acoustic isolation at the wintering grounds. As with the correlations in humans between genes, communication and migration, the migration patterns of humpback whales are written into their songs.

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32

KOMAI, TOMOYUKI, and TIN-YAM CHAN. "A new genus and two new species of alvinocaridid shrimps (Crustacea: Decapoda: Caridea) from a hydrothermal vent field off northeastern Taiwan." Zootaxa 2372, no. 1 (February 26, 2010): 15–32. http://dx.doi.org/10.11646/zootaxa.2372.1.3.

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Two new species of alvinocaridid shrimps are described from a hydrothermal vent field off northeastern Taiwan at depths of 252–300 m. Alvinocaris chelys n. sp. is morphologically very similar to A. williamsi Shank & Martin, 2003 from the Mid-Atlantic Ridge, and A. alexander Ahyong, 2009 from the southern Kermadec Ridge. These three species can be differentiated by the shape of the postrostral ridge, telson, the second segment of the antennular peduncle and the armature of the meri and ischia of the third pereopod. The second new species, although rather similar to Alvinocaris niwa Webber, 2004 from the Kermadec-Arc, is assigned to a new genus Alvinocaridinides gen. nov., which appears to be intermediate between Shinkaicaris Komai & Segonzac, 2005 and other derived genera including Opaepele Williams & Dobbs, 1995, Chorocaris Martin & Hessler, 1990 and Rimicaris Williams & Rona, 1986. Alvinocaridinides formosa n. sp. differs from Alvinocaris niwa by completely lacking any armature on the ischia of the third to fifth pereopods and by bearing two movable spines at the posterolateral angle of the uropodal exopod. These records constitute the first discovery of the family Alvinocarididae in Taiwanese waters and represent the shallowest occurrence for alvinocaridid shrimps.

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33

Fujiwara, Kyoji, Kevin W. Conway, and Hiroyuki Motomura. "First record of the Kermadec Clingfish, Flexor incus Conway, Stewart & Summers, 2018 (Gobiesocidae), from New Caledonia and Australia." Check List 17, no. 3 (May 14, 2021): 769–73. http://dx.doi.org/10.15560/17.3.769.

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Two specimens (17.1 and 29.1 mm standard length) of Flexor incus Conway, Stewart & Summers, 2018 (Gobiesocidae) were collected from New Caledonia and Lord Howe Island, Australia. The species and genus were originally described on the basis of 15 specimens from the Kermadec Islands, New Zealand, where the genus has been considered endemic. The two specimens reported herein represent the first records of F. incus from New Caledonia and Australia.

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34

SCHNABEL, KAREEN E., and NIEL L. BRUCE. "New records of Munidopsis (Crustacea: Anomura: Galatheidae) from New Zealand with description of two new species from a seamount and underwater canyon." Zootaxa 1172, no. 1 (April 13, 2006): 49. http://dx.doi.org/10.11646/zootaxa.1172.1.5.

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Three species of the genus Munidopsis are currently known from New Zealand waters: M. marginata (Henderson, 1885), M. kaiyoae Baba, 1974 and M. abyssicola Baba, 2005. New records for M. marginata and M. kaiyoae around New Zealand are provided and Munidopsis maunga n. sp. and M. papanui n. sp. are described from a seamount on the Kermadec volcanic arc and the Papanui canyon off the southeast coast of New Zealand, respectively.

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35

WEBBER, W. RICHARD. "A new species of Alvinocaris (Crustacea: Decapoda: Alvinocarididae) and new records of alvinocaridids from hydrothermal vents north of New Zealand." Zootaxa 444, no. 1 (March 1, 2004): 1. http://dx.doi.org/10.11646/zootaxa.444.1.1.

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Alvinocaris niwa n. sp. is described from hydrothermal vents at the Brothers Caldera and Rumble V Seamount on the southern Kermadec Ridge, midway between the Kermadec Islands and Bay of Plenty, New Zealand. Four hundred specimens of Alvinocaris longirostris Kikuchi & Ohta, 1995, described from Japan, are recorded at the Brothers. The presence of a possible third Alvinocaris at Rumble V and one or two species of Chorocaris at Brothers are also reported. Eighty-eight specimens of A. niwa and 41 of A. longirostris were measured and examined to assess morphological variation. Morphological characters used to distinguish alvinocaridids are shown to be highly variable. Pairwise correlations with carapace length indicate that numbers of teeth, spines and setae are generally not related to shrimp size. Descriptions based on small numbers of specimens are thus questionable. The new species is characterised by: short rostrum; paired sternal spines on abdominal somites I III; long stylocerite and robust distolateral spine on the antennular proximal segment, with a subterminal spine; two ventral spines on antennal basal segment; row of spines on distal segment of maxilliped III; and two rows of spines on flexor surface of P3 P5 dactyls. It is the shallowest alvinocaridid yet discovered and also inhabits the greatest depth range, at over 700 m.

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Spencer, Hamish G., Jonathan M. Waters, and Thomas E. Eichhorst. "Taxonomy and nomenclature of black nerites (Gastropoda:Neritimorpha:Nerita) from the South Pacific." Invertebrate Systematics 21, no. 3 (2007): 229. http://dx.doi.org/10.1071/is06038.

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Members of the genus Nerita are abundant components of the intertidal fauna in many parts of the world and yet Nerita taxonomy remains unsettled. Here, the relationships among black-shelled Nerita populations from Australia, New Zealand, Norfolk Island, Lord Howe Island, the Kermadec Islands and Easter Island are discussed. Four species are recognised: N. atramentosa Reeve, 1855 from the southern half of Australia; N. melanotragus E.A. Smith, 1884 from eastern Australia, northern New Zealand, Lord Howe Island, Norfolk Island and the Kermadec Islands; N. morio (G. B. Sowerby I, 1833) from Easter Island and the Austral Islands; and N. lirellata Rehder, 1980 from Easter Island alone. These species are of great importance in studies of intertidal community structure and yet two of them have been consistently confused in the ecological and taxonomic literature. Moreover, the relationships among the species are not at all as implied by recent subgeneric classifications; it is argued that all four species should be placed in the subgenus Lisanerita Krijnen, 2002. The superficially similar N. picea Récluz, 1841 is not closely related. An accurate taxonomy of the genus will almost certainly require considerable genetic analysis. The nomenclature for each species is herein established by complete synonymies, and lectotypes for both N. atramentosa and N. melanotragus are selected.

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Francis, Malcolm P., David Harasti, and Hamish A. Malcolm. "Surviving under pressure and protection: a review of the biology, ecology and population status of the highly vulnerable grouper Epinephelus daemelii." Marine and Freshwater Research 67, no. 8 (2016): 1215. http://dx.doi.org/10.1071/mf15099.

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Epinephelus daemelii is a threatened serranid grouper species that is restricted to the south-western Pacific Ocean, ranging from eastern Australia to northern New Zealand and the Kermadec Islands. Declines in its abundance due to fishing pressure were reported as early as 1916. Aspects of this species’ biology and behaviour that make it vulnerable include its longevity, late age at maturity, protogynous hermaphroditism, territoriality and limited shallow reef habitat. Adults prefer complex habitat with caves and overhangs at depths of less than 50m, whereas juveniles live in rock pools, shallow intertidal reefs and estuaries. Epinephelus daemelii lives at least 65 years and reaches 170-cm total length. Individuals change sex from female to male at ~100–110cm and ~25 years. Absence of large (>100cm) fish across a large part of their range has implications for reproduction. Although nearly fully protected, incidental bycatch still occurs. A lack of long-term data hinders determination of population status, but abundance appears to be much lower than before, except in remote regions (Kermadec Islands, Elizabeth and Middleton reefs) with extensive no-fishing areas. Further prohibitions on fishing in key locations are likely to be important for the recovery and long-term survival of this species.

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Collot, J., M. Patriat, R. Sutherland, S. Williams, D. Cluzel, M. Seton, B. Pelletier, et al. "Chapter 2 Geodynamics of the SW Pacific: a brief review and relations with New Caledonian geology." Geological Society, London, Memoirs 51, no. 1 (2020): 13–26. http://dx.doi.org/10.1144/m51-2018-5.

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AbstractThe SW Pacific region consists of a succession of ridges and basins that were created by the fragmentation of Gondwana and the evolution of subduction zones since Mesozoic times. This complex geodynamic evolution shaped the geology of New Caledonia, which lies in the northern part of the Zealandia continent. Alternative tectonic models have been postulated. Most models agree that New Caledonia was situated on an active plate margin of eastern Gondwana during the Mesozoic. Extension affected the region from the Late Cretaceous to the Paleocene and models for this period vary in the location and nature of the plate boundary between the Pacific and Australian plates. Eocene regional tectonic contraction included the obduction of a mantle-derived Peridotite Nappe in New Caledonia. In one class of model, this contractional phase was controlled by an east-dipping subduction zone into which the Norfolk Ridge jammed, whereas and in a second class of model this phase corresponds to the initiation of the west-dipping Tonga–Kermadec subduction zone. Neogene tectonics of the region near New Caledonia was dominated by the eastwards retreat of Tonga–Kermadec subduction, leading to the opening of a back-arc basin east of New Caledonia, and the initiation and southwestwards advance of the New Hebrides–Vanuatu subduction zone towards New Caledonia.

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de Ronde, C. E. J., D. A. Butterfield, and M. I. Leybourne. "Metallogenesis and Mineralization of Intraoceanic Arcs I: Kermadec Arc--Introduction." Economic Geology 107, no. 8 (November 23, 2012): 1521–25. http://dx.doi.org/10.2113/econgeo.107.8.1521.

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Timm, C., C. E. J. de Ronde, M. I. Leybourne, D. Layton-Matthews, and I. J. Graham. "Sources of Chalcophile and Siderophile Elements in Kermadec Arc Lavas." Economic Geology 107, no. 8 (November 23, 2012): 1527–38. http://dx.doi.org/10.2113/econgeo.107.8.1527.

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41

Nelson, Wendy, Clinton Duffy, Thomas Trnski, and Rob Stewart. "Mesophotic Ecklonia radiata (Laminariales) at Rangitāhua, Kermadec Islands, New Zealand." Phycologia 57, no. 5 (September 2018): 534–38. http://dx.doi.org/10.2216/18-9.1.

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Lundgren, Paul R., Emile A. Okal, and Douglas A. Wiens. "Rupture characteristics of the 1982 Tonga and 1986 Kermadec earthquakes." Journal of Geophysical Research: Solid Earth 94, B11 (November 10, 1989): 15521–39. http://dx.doi.org/10.1029/jb094ib11p15521.

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Suetsugu, Daisuke. "Defocusing of teleseismic P-waves by the Tonga-Kermadec Slab." Geophysical Research Letters 26, no. 18 (September 15, 1999): 2785–88. http://dx.doi.org/10.1029/1998gl005307.

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Nunnally, Clifton C., Jason R. Friedman, and Jeffrey C. Drazen. "In situ respiration measurements of megafauna in the Kermadec Trench." Deep Sea Research Part I: Oceanographic Research Papers 118 (December 2016): 30–36. http://dx.doi.org/10.1016/j.dsr.2016.10.009.

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Hirose, Fuyuki, Kenji Maeda, and Osamu Kamigaichi. "Tidal Forcing of Interplate Earthquakes Along the Tonga‐Kermadec Trench." Journal of Geophysical Research: Solid Earth 124, no. 10 (October 2019): 10498–521. http://dx.doi.org/10.1029/2019jb018088.

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46

Peoples, Logan M., Sierra Donaldson, Oladayo Osuntokun, Qing Xia, Alex Nelson, Jessica Blanton, Eric E. Allen, Matthew J. Church, and Douglas H. Bartlett. "Vertically distinct microbial communities in the Mariana and Kermadec trenches." PLOS ONE 13, no. 4 (April 5, 2018): e0195102. http://dx.doi.org/10.1371/journal.pone.0195102.

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Smith, I. E. M., and R. N. Brothers. "Petrology of the Rumble seamounts, southern Kermadec Ridge, southwest Pacific." Bulletin of Volcanology 50, no. 3 (June 1988): 139–47. http://dx.doi.org/10.1007/bf01079678.

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Houston, Heidi, Helen Anderson, Susan L. Beck, Jiajun Zhang, and Susan Schwartz. "The 1986 Kermadec earthquake and its relation to plate segmentation." Pure and Applied Geophysics PAGEOPH 140, no. 2 (1993): 331–64. http://dx.doi.org/10.1007/bf00879411.

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BUCKERIDGE, JOHN S. "Ashinkailepas kermadecensis, a new species of deep-sea scalpelliform barnacle (Thoracica: Eolepadidae) from the Kermadec Islands, southwest Pacific." Zootaxa 2021, no. 1 (February 27, 2009): 57–65. http://dx.doi.org/10.11646/zootaxa.2021.1.4.

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A new deep-sea stalked barnacle, Ashinkailepas kermadecensis sp. nov. has been recovered from a cold-water seep at depths of 1165 metres in the vicinity of the Kermadec Ridge to the northeast of the North Island, New Zealand. There are now two species of Ashinkailepas—the other, Ashinkailepas seepiophila Yamaguchi, Newman & Hashimoto, 2004, occurs in deep, cold seeps off central Japan. As there are two species within Ashinkailepas, formal diagnoses are provided for both taxa.

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Leybourne, M. I., U. Schwarz-Schampera, C. E. J. de Ronde, E. T. Baker, K. Faure, S. L. Walker, D. A. Butterfield, et al. "Submarine Magmatic-Hydrothermal Systems at the Monowai Volcanic Center, Kermadec Arc." Economic Geology 107, no. 8 (November 23, 2012): 1669–94. http://dx.doi.org/10.2113/econgeo.107.8.1669.

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