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Journal articles on the topic 'Heard Island'

Author: Grafiati

Published: 4 June 2021

Last updated: 21 February 2023

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1

Slip, David J., and Harry R. Burton. "Accumulation of Fishing Debris, Plastic Litter, and Other Artefacts, on Heard and Macquarie Islands in the Southern Ocean." Environmental Conservation 18, no. 3 (1991): 249–54. http://dx.doi.org/10.1017/s0376892900022177.

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Sections of coastline of Heard and Macquarie Islands were surveyed for marine debris in the summer of 1987–88 and 1989, respectively. These surveys were carried out at the same sites as previous surveys in 1986–87 at Heard Island, and in 1988 at Macquarie Island. The minimum rate of artefact accumulation was 13 objects per km of shoreline per year for Heard Island, and 90 objects per km of shoreline per year for Macquarie Island. Drift-cards, released from known locations and collected on the two islands, show a similar artefact catchment area.Plastic litter was a major component of the debris

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2

Smith, J. M. B., P. Rudall, and P. L. Keage. "Driftwood on Heard Island." Polar Record 25, no. 154 (1989): 223–28. http://dx.doi.org/10.1017/s0032247400010834.

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AbstractSamples from 73 pieces of non-structural driftwood on Heard Island (53°06′S, 73°30′E) were identified to genus or species. Thirty-one belonged to South American species of Nothofagus. The remainder, consisting mostly of conifers especially Picea and Larix, probably came from ships' cargoes. The assemblage is similar to those reported, from smaller samples, on other southern islands. Other items of flotsam, including fishing buoys and drift-cards, are also reported from Heard Island. The significance of driftwood transport from South America to the island in accounting for long-distance

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3

Briscoe, M. G. "The Heard Island global program: Today Heard Island, tomorrow the world." Journal of the Acoustical Society of America 90, no. 4 (1991): 2329. http://dx.doi.org/10.1121/1.402236.

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4

E. Davis. Jr., William. "Heard Island: Southern Ocean Sentinel." Pacific Conservation Biology 13, no. 2 (2007): 145. http://dx.doi.org/10.1071/pc070145.

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Heard Island is one of the most remote places on earth. It is of volcanic origin (and currently volcanically active) on the submarine Kerguelen Plateau in the Southern Ocean, roughly 4 000 km south-west of Australia, 1 500 km from Antarctica, 3 750 km from Africa, and 7 500 km from India. The island is 367 km2 in area at latitude 53�S, south of the Antarctic Polar Front (Antarctic Convergence), is 70% covered with glaciers, and has a geologic, biologic and human history of substantial interest. Because of its remoteness, relative recent discovery (1853), and infrequent human visitation, it is

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5

Williams, R., and G. Duhamel. "Volcanic activity on Heard Island." Polar Record 23, no. 142 (1986): 88–90. http://dx.doi.org/10.1017/s0032247400006884.

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6

Spindel, Robert. "Heard Island global warming test." Environmental Science & Technology 25, no. 2 (1991): 210–12. http://dx.doi.org/10.1021/es00014a600.

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7

Greenslade, Penelope, P. Vernon, and D. Smith. "Ecology of Heard Island Diptera." Polar Biology 35, no. 6 (2011): 841–50. http://dx.doi.org/10.1007/s00300-011-1128-5.

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8

Munk, Walter H., Robert C. Spindel, Arthur Baggeroer, and Theodore G. Birdsall. "The Heard Island Feasibility Test." Journal of the Acoustical Society of America 96, no. 4 (1994): 2330–42. http://dx.doi.org/10.1121/1.410105.

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9

Baggeroer, Arthur, and Walter Munk. "The Heard Island Feasibility Test." Physics Today 45, no. 9 (1992): 22–30. http://dx.doi.org/10.1063/1.881317.

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10

Allison, Ian F., and Peter L. Keage. "Recent changes in the glaciers of Heard Island." Polar Record 23, no. 144 (1986): 255–72. http://dx.doi.org/10.1017/s0032247400007099.

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ABSTRACTHeard Island, a heavily glacierized volcanic island in the Southern Ocean, is 80% ice-covered, with glaciers descending from 2,400 m to sea level: major glaciers are up to 7 km long with areas exceeding 10 km. Much of the island was photographed from the air in 1947 and again in early 1980. Photographs and limited ground surveys record changes (mostly retreats) in glacier fronts. Retreat is most marked on the eastern flanks where former tidewater glaciers are now grounded inland. Glaciers on northern and windward western flanks still end in ice cliffs but have narrowed; glaciers and ic

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11

Greenslade, Penelope, and L. Deharveng. "Revision of Friesea Species (Collembola: Neanuridae) of Australia and Offshore Islands, with Biogeographical Notes and Key to Species." Invertebrate Systematics 11, no. 2 (1997): 321. http://dx.doi.org/10.1071/it95033.

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Seven species of Friesea are recorded here from Australia and its offshore islands and a key and checklist is provided to them. Three of the species, F. neptunia, F. australica and F. florifera, are new and are described here, and one, F. bispinosa Deharveng, from Heard and Macquarie Islands, is a new record for Australia. Earlier records of F. mirabilis Tullberg and F. claviseta Axelson are examined and the seventh species, F. tilbrooki Wise, already recorded from Macquarie Island and Heard Island, is probably a synonym of F. multispinosa Denis from Kerguelen. Records of Friesea sp. cf. clavi

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12

Budd, Grahame M. "Australian exploration of Heard Island, 1947–1971." Polar Record 43, no. 2 (2007): 97–123. http://dx.doi.org/10.1017/s0032247407006080.

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In 1947 knowledge of Heard Island was confined to a rough mapping compiled by nineteenth-century sealers, and the results of four scientific expeditions that had briefly investigated the Atlas Cove area. Exploration continued in two distinct periods between 1947 and 1971. In the first period the Australian National Antarctic Research Expeditions (ANARE) built a scientific station at Atlas Cove in 1947, and occupied it continuously until 1955 as an ‘A Class’ meteorological station, a seismic and magnetic observatory, and a base for other scientific studies and for exploration of the island. In

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13

Burenkov, S. V., A. N. Gavrilov, A. Y. Uporin, and A. V. Furduev. "Heard Island feasibility test: Long‐range sound transmission from Heard Island to Krylov underwater mountain." Journal of the Acoustical Society of America 90, no. 4 (1991): 2330–31. http://dx.doi.org/10.1121/1.402241.

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14

Burenkov, S. V., A. N. Gavrilov, A. Y. Uporin, and A. V. Furduev. "Heard Island Feasibility Test: Long‐range sound transmission from Heard Island to Krylov underwater mountain." Journal of the Acoustical Society of America 96, no. 4 (1994): 2458–63. http://dx.doi.org/10.1121/1.410118.

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15

Øvstedal, D. O., and N. J. M. Gremmen. "Lichens of sub-Antarctic Heard Island." South African Journal of Botany 72, no. 3 (2006): 353–66. http://dx.doi.org/10.1016/j.sajb.2005.09.008.

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16

Marshall, David J., and Steven L. Chown. "The acarine fauna of Heard Island." Polar Biology 25, no. 9 (2002): 688–95. http://dx.doi.org/10.1007/s00300-002-0404-9.

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17

Munk, Walter. "Acoustics 1993: Heard Island and beyond." Journal of the Acoustical Society of America 95, no. 1 (1994): 567. http://dx.doi.org/10.1121/1.408352.

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18

Rootes, David. "Possible World Heritage listing for Heard Island and the McDonald Islands." Polar Record 27, no. 162 (1991): 256. http://dx.doi.org/10.1017/s0032247400012687.

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19

Bergstrom, Dana, and Patricia Selkirk. "Distribution of Bryophytes on Subantarctic Heard Island." Bryologist 100, no. 3 (1997): 349. http://dx.doi.org/10.1639/0007-2745(1997)100[349:dobosh]2.0.co;2.

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20

Bergstrom, Dana, and Patricia Selkirk. "Distribution of Bryophytes on Subantarctic Heard Island." Bryologist 100, no. 3 (1997): 349. http://dx.doi.org/10.2307/3244503.

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21

Bergstrom, Dana M., Jennie Whinam, and Lee Belbin. "A Classification of Subantarctic Heard Island Vegetation." Arctic, Antarctic, and Alpine Research 34, no. 2 (2002): 169. http://dx.doi.org/10.2307/1552468.

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22

Bergstrom, Dana M., Jennie Whinam, and Lee Belbin. "A Classification of Subantarctic Heard Island Vegetation." Arctic, Antarctic, and Alpine Research 34, no. 2 (2002): 169–77. http://dx.doi.org/10.1080/15230430.2002.12003481.

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23

Sanga, Kabini, and Martyn Reynolds. "Whose voice is heard?" New Zealand Annual Review of Education 27 (November 24, 2022): 44–59. http://dx.doi.org/10.26686/nzaroe.v27.8031.

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Aotearoa New Zealand has had a long association with other states in the Pacific, notably with Pacific Island countries generally grouped as Polynesia and Melanesia. Donor-aid and the introduced ideas of consultants have been currencies in many of these well-appreciated relationships. However, more collaborative arrangements have also born significant fruit. These include the collaborative publications of the now dis-established He Pārekereke Institute for Research and Development in Māori and Pacific Education. This article offers a sketch of the potential of He Pārekereke as an example of a

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24

Selkirk, P. M., J. P. Whinam, A. J. Downing, and M. L. Skotnicki. "Mosses of sub-Antarctic Heard Island: an updated list and discussion of their distribution." Polar Record 44, no. 2 (2008): 155–64. http://dx.doi.org/10.1017/s003224740700722x.

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ABSTRACTDuring an early summer visit in 2000, mosses were collected from sites around Heard Island. Three species, Bryoerythrophyllum recurvirostrum (Hedw.) P.C.Chen, Philonotis cf. tenuis (Taylor) Reichardt and Syntrichia filaris (Müll.Hall) R.H. Zander have been added to the list of moss species known from the island, bringing the total to 40 moss taxa. Syntrichia anderssonii (abcngström) R.H. Zander was found with sporophytes, whereas previously its sporophytes were known in the sub-Antarctic only from Macquarie Island. Extensions of range on Heard Island have been recorded for several spec

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25

Green, K., H. R. Burton, and R. Williams. "The diet of Antarctic fur seals Arctocephalus gazella (Peters) during the breeding season at Heard Island." Antarctic Science 1, no. 4 (1989): 317–24. http://dx.doi.org/10.1017/s0954102089000489.

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Between September 1987 and February 1988, Antarctic fur seals Arctocephalus gazella (Peters) at Heard Island fed mainly on fish with an average 95.2% of scats in monthly collections containing fish remains. Pelagic myctophids constituted more than 50% of fish taken by fur seals at the beginning of the summer season and again at the end when there was an influx of non-breeding male seals. During the middle period from October to December, fish from the surrounding shelf area comprised the bulk of the diet. These included various benthic nototheniid species, the bentho-pelagic ice fish Champsoce

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26

Patrick, Matthew R., and John L. Smellie. "Synthesis A spaceborne inventory of volcanic activity in Antarctica and southern oceans, 2000–10." Antarctic Science 25, no. 4 (2013): 475–500. http://dx.doi.org/10.1017/s0954102013000436.

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AbstractOf the more than twenty historically active volcanoes in Antarctica and the sub-Antarctic region only two, to our knowledge, host any ground-based monitoring instruments. Moreover, because of their remoteness, most of the volcanoes are seldom visited, thus relegating the monitoring of volcanism in this region almost entirely to satellites. In this study, high temporal resolution satellite data from the Hawaii Institute of Geophysics and Planetology's MODVOLC system using MODIS (Moderate Resolution Imaging Spectroradiometer) are complemented with high spatial resolution data (ASTER, or

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27

KIERNAN, KEVIN, and ANNE McCONNELL. "Geomorphology of the Sub-Antarctic Australian Territory of Heard Island-McDonald Island." Australian Geographer 30, no. 2 (1999): 159–95. http://dx.doi.org/10.1080/00049189993693.

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28

Yan, Jianguo, and Kang K. Yen. "Horizontal ray paths of underwater sound from Heard Island to Ascension Island." Applied Acoustics 45, no. 1 (1995): 9–18. http://dx.doi.org/10.1016/0003-682x(94)00025-q.

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29

Scott, J. J. "New records of vascular plants from Heard Island." Polar Record 25, no. 152 (1989): 37–42. http://dx.doi.org/10.1017/s0032247400009967.

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AbstractEight species of vascular plants were previously known from subantarctic Heard Island. Three additional species, Montia fontana, Ranunculus biternatus and Poa annua, were discovered during the 1986 austral summer. Details of their habitat and known distribution on the island, and their possible means of arrival, are discussed.

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30

Potter, Sandra. "The Quarantine Protection of Sub-Antarctic Australia: Two Islands, Two Regimes." Island Studies Journal 2, no. 2 (2007): 177–92. http://dx.doi.org/10.24043/isj.206.

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Sub-Antarctic Heard Island and Macquarie Island are among Australia’s offshore properties susceptible to colonization by species introduced by humans. While both islands share World Heritage status and are IUCN Category Ia Protected Areas (Strict Nature Reserves), different quarantine protection regimes are in operation. Macquarie Island’s biosecurity appears to be less catered for while the means and likelihood of introductions are greater. The administrative, political, practical and geographical contexts within which quarantine management planning takes place variously impact on the level o

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31

Spindel, Robert C. "The Heard Island acoustic global warming feasibility test." Journal of the Acoustical Society of America 90, no. 4 (1991): 2328. http://dx.doi.org/10.1121/1.402234.

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32

Duncan, R. A., P. G. Quilty, J. Barling, and J. M. Fox. "Geological development of Heard Island, Central Kerguelen Plateau." Australian Journal of Earth Sciences 63, no. 1 (2016): 81–89. http://dx.doi.org/10.1080/08120099.2016.1139000.

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33

Goldsworthy, S. D., and P. D. Shaughnessy. "Subantarctic fur seals Arctocephalus tropicalis at Heard Island." Polar Biology 9, no. 5 (1989): 337–39. http://dx.doi.org/10.1007/bf00287434.

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34

Smith, J. M. B., and R. D. Simpson. "Biotic zonation on rocky shores of Heard Island." Polar Biology 4, no. 2 (1985): 89–94. http://dx.doi.org/10.1007/bf00442905.

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35

Thost, Douglas E., and Martin Truffer. "Glacier Recession on Heard Island, Southern Indian Ocean." Arctic, Antarctic, and Alpine Research 40, no. 1 (2008): 199–214. http://dx.doi.org/10.1657/1523-0430(06-084)[thost]2.0.co;2.

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36

Baggeroer, Arthur B., Brian Sperry, Khosrow Lashkari, et al. "Vertical array receptions of the Heard Island transmissions." Journal of the Acoustical Society of America 96, no. 4 (1994): 2395–413. http://dx.doi.org/10.1121/1.410112.

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37

Brundrit, G. B., and L. Krige. "Heard Island signals through the Agulhas retroflection region." Journal of the Acoustical Society of America 96, no. 4 (1994): 2464–68. http://dx.doi.org/10.1121/1.410119.

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38

ØVSTEDAL, D. O., and N. J. M. GREMMEN. "Additions and corrections to the lichens of Heard Island." Lichenologist 40, no. 3 (2008): 233–42. http://dx.doi.org/10.1017/s002428290800741x.

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Abstract:Nineteen lichens new to sub-Antarctic Heard Island are recorded. Three species are described as new: Gyalideopsis heardense Øvstedal, Mycobilimbia subbyssoidea Øvstedal and Psoroma absconditum Øvstedal. Altogether the total number of lichen species recorded on the island is now 90.

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39

Spencer, Mary Jo, Paul A. Mayewski, Wm Berry Lyons, and Martin R. Hendy. "A Preliminary Assessment of the Potential Application of Glaciochemical Investigations on Heard Island South Indian Ocean." Journal of Glaciology 31, no. 109 (1985): 233–36. http://dx.doi.org/10.1017/s0022143000006559.

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AbstractAnalyses of fluoride, chloride, sodium, sulfate, bromide, nitrate, and iron from a 3 m snow pit on Heard Island, collected at an elevation of 2450, m are used to assess the potential of glaciochemical studies on. Heard Island glaciers. Sources for the chemical species are identified and, in particular, chloride, sodium, and sulfate are found to be useful seasonal indicators. The total record measured is believed to be less than one mass-balance year.

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40

Spencer, Mary Jo, Paul A. Mayewski, Wm Berry Lyons, and Martin R. Hendy. "A Preliminary Assessment of the Potential Application of Glaciochemical Investigations on Heard Island, South Indian Ocean." Journal of Glaciology 31, no. 109 (1985): 233–36. http://dx.doi.org/10.3189/s0022143000006559.

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AbstractAnalyses of fluoride, chloride, sodium, sulfate, bromide, nitrate, and iron from a 3 m snow pit on Heard Island, collected at an elevation of 2450, m are used to assess the potential of glaciochemical studies on. Heard Island glaciers. Sources for the chemical species are identified and, in particular, chloride, sodium, and sulfate are found to be useful seasonal indicators. The total record measured is believed to be less than one mass-balance year.

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41

Barling, J., S. L. Goldstein, G. E. Wheller, and I. A. Nicholls. "Heard Island: An example of large isotopic variations on a small Oceanic Island." Chemical Geology 70, no. 1-2 (1988): 46. http://dx.doi.org/10.1016/0009-2541(88)90305-1.

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42

FRYDAY, Alan M. "New species and combinations in Calvitimela and Tephromela from the southern subpolar region." Lichenologist 43, no. 3 (2011): 225–39. http://dx.doi.org/10.1017/s0024282911000065.

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AbstractThe new species Calvitimela austrochilenis Fryday and Tephromela superba Fryday are described: the former from several collections from southern Chile and one from Marion Island, and the latter from southern South America (including the Falkland Islands), Campbell Island, (New Zealand), and Antarctica. Four new combinations are also made in Tephromela: T. atrocaesia (Nyl. ex Cromb.) Fryday from Îles Kerguelen, Heard Island, South Georgia, and southern South America; T. atroviolacea (Flot.) Fryday from southern South America and Îles Kerguelen; T. lirellina (Darb.) Fryday from only sout

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43

STEPHENSON, JON, G. M. BUDD, J. MANNING, and P. HANSBRO. "Major eruption-induced changes to the McDonald Islands, southern Indian Ocean." Antarctic Science 17, no. 2 (2005): 259–66. http://dx.doi.org/10.1017/s095410200500266x.

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The McDonald Islands (53°S, 73°E) originally comprised three small islands that lie on the Kerguelen Plateau, 44 km west of Heard Island. No volcanic activity was observed since their discovery in 1874 until 1997, when two passing ships recorded major changes and eruptive behaviour. A 2001 satellite image showed that the main island had doubled its area. This paper reports observations made from a cruise ship in November 2002, supplemented by a high-resolution satellite image acquired in March 2003. A new volcanic complex comprises lava domes, spines and flows, all assumed to be phonolitic, si

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44

Hoff, John van den, Rupert Davies, and Harry Burton. "Origins, age composition and change in numbers of moulting southern elephant seals (Mirounga leonina L.) in the Windmill Islands, Vincennes Bay, east Antarctica, 1988 - 2001." Wildlife Research 30, no. 3 (2003): 275. http://dx.doi.org/10.1071/wr01086.

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We discovered that the number of male southern elephant seals (Mirounga leonina) moulting at wallow sites in the Windmill Islands, Vincennes Bay, Antarctica has decreased by 88% since the last data were presented in 1989. This figure equates to an annual decrease of 6.5%, a figure quite different to the known population trends at the islands from where the seals originate. The seals inhabited four fewer wallows in 2001 than in 1990. Brand and tag resights confirm that seals moulting at Browning Peninsula and Peterson Island originate from Macquarie Island and Heard Island. Male seals aged 1–7+

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45

Green, K., and L. A. Mound. "An extension to the insect fauna of Heard Island." Polar Record 30, no. 173 (1994): 131–32. http://dx.doi.org/10.1017/s0032247400021343.

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The insect fauna of Heard Island were investigated on the ChallengerExpedition in 1875 (Kirby 1884); the Deutsche Sudpolar-Expedition in 1902 (VanHöffen 1912); and the Australian National Antarctic Research Expedition in 1951/52(Brown 1964; Gressitt and Temple 1970; Home 1984). With the addition of Lepidoptera in these last reports, six orders of insects were recognised as occurring on Heard Island, the others being Collembola, Coleoptera, Diptera, Siphonaptera, and Mallophaga. The present note reports the addition of a seventh order, Thysanoptera, to the fauna.

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46

Green, K., R. Williams, E. J. Woehler, H. R. Burton, N. J. Gales, and R. T. Jones. "Diet of the Heard Island cormorant Phalacrocorax atriceps nivalis." Antarctic Science 2, no. 2 (1990): 139–41. http://dx.doi.org/10.1017/s0954102090000177.

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The diet of Heard Island cormorants was investigated by examination of casts over three summer seasons. The diet was composed mainly of benthic organisms, with polychaetes being the most common prey for the greater part of the population. Fish were taken commonly only by the small breeding population at the western end of the island, whereas elsewhere only 22% of casts contained any fish remains at all. The diet is therefore different from that reported for Phalacrocorax atriceps at other localities.

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47

Whinam, J., P. M. Selkirk, A. J. Downing, and Bruce Hull. "Return of the megaherbs: plant colonisation of derelict ANARE station buildings on sub-Antarctic Heard Island." Polar Record 40, no. 3 (2004): 235–43. http://dx.doi.org/10.1017/s0032247404003614.

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Buildings were constructed and artefacts left behind on sub-Antarctic Heard Island, associated with Antarctic research expeditions since 1926. Both bryophytes and vascular plants are colonising many parts of the now derelict buildings. On these structures and artefacts, the authors recorded four species of vascular plants out of the 11 that occur on Heard Island and nine species of mosses out of the 37 recorded from Heard Island. The vascular plant species most frequently recorded colonising structures and artefacts was Pringlea antiscorbutica (288 occurrences), with the area colonised varying

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48

Brundrit, G. B., R. C. van Ballegooyen, H. R. Valentine, et al. "Reception of the Heard Island signals off South Africa." Journal of the Acoustical Society of America 90, no. 4 (1991): 2347. http://dx.doi.org/10.1121/1.402195.

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49

Munk, Walter, and Arthur Baggeroer. "The Heard Island papers: A contribution to global acoustics." Journal of the Acoustical Society of America 96, no. 4 (1994): 2327–29. http://dx.doi.org/10.1121/1.411316.

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50

Van de Vijver, Bart, Louis Beyens, Sofie Vincke, and Niek J. M. Gremmen. "Moss-inhabiting diatom communities from Heard Island, sub-Antarctic." Polar Biology 27, no. 9 (2004): 532–43. http://dx.doi.org/10.1007/s00300-004-0629-x.

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