Academic literature on the topic 'Erosion – Tasmania – Macquarie Island'

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Journal articles on the topic "Erosion – Tasmania – Macquarie Island"

1

Banks, Maxwell R., Eric A. Colhoun, and David Hannan. "Early Discoveries of the Effects of Ice Action in Australia." Journal of Glaciology 33, no. 114 (1987): 231–35. http://dx.doi.org/10.1017/s002214300000873x.

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Abstract The effects of past glaciation in what is now Australian territory were first recognized on Macquarie Island, probably by David Ramsay, in 1821. The recognition by Darwin in 1836, and reporting by Milligan in 1848 of ice-transported pebbles and boulders in late Palaeozoic marine rocks in Tasmania, showed on the one hand participation in and on the other familiarity with the controversy in Great Britain at that time on the origin of erratics and drift currents. Reports by Clarke (1852), Daintree in 1859, Selwyn (1860), and Gould (1860) of the effects of land ice on Mount Koscuisko (New South Wales), Bacchus Marsh (Victoria), Inman Valley (South Australia), and the Central Highlands (Tasmania), respectively, reflect the increasing recognition in Great Britain of the erosional and depositional effects of glaciers. Daintree, Selwyn, and Gould were all closely connected with A.C. Ramsay, the main British protagonist of the glacial theory at the time, whereas David Ramsay and Milligan were probably influenced by Robert Jameson of Edinburgh.
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2

Banks, Maxwell R., Eric A. Colhoun, and David Hannan. "Early Discoveries of the Effects of Ice Action in Australia." Journal of Glaciology 33, no. 114 (1987): 231–35. http://dx.doi.org/10.3189/s002214300000873x.

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AbstractThe effects of past glaciation in what is now Australian territory were first recognized on Macquarie Island, probably by David Ramsay, in 1821. The recognition by Darwin in 1836, and reporting by Milligan in 1848 of ice-transported pebbles and boulders in late Palaeozoic marine rocks in Tasmania, showed on the one hand participation in and on the other familiarity with the controversy in Great Britain at that time on the origin of erratics and drift currents. Reports by Clarke (1852), Daintree in 1859, Selwyn (1860), and Gould (1860) of the effects of land ice on Mount Koscuisko (New South Wales), Bacchus Marsh (Victoria), Inman Valley (South Australia), and the Central Highlands (Tasmania), respectively, reflect the increasing recognition in Great Britain of the erosional and depositional effects of glaciers. Daintree, Selwyn, and Gould were all closely connected with A.C. Ramsay, the main British protagonist of the glacial theory at the time, whereas David Ramsay and Milligan were probably influenced by Robert Jameson of Edinburgh.
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3

Stephenson, Steven L., Gary A. Laursen, and Rodney D. Seppelt. "Myxomycetes of subantarctic Macquarie Island." Australian Journal of Botany 55, no. 4 (2007): 439. http://dx.doi.org/10.1071/bt06169.

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Macquarie Island is an oceanic island located 1000 km south-east of Tasmania. The island, which lies close to but north of the Antarctic Convergence, is the southernmost island in the world with a fairly complete cover of vegetation. However, the vascular flora is impoverished and consists of only 46 species. During the period of late January to late April of 1995, 412 field collections of myxomycetes, representing at least 22 species in 11 genera, were obtained during the course of an intensive survey of fungal biodiversity on Macquarie Island. Moist-chamber cultures prepared with various types of plant debris yielded only 14 collections, but this total included three additional species and two additional genera. All but four of the species we recorded from the island are new records for the South Polar Region. Most field collections were associated with Stilbocarpa polaris (Araliaceae) and Pleurophyllum hookeri (Asteraceae), the usual dominants in the herbfield communities that commonly occur on upper beach slopes and coastal terraces. Trichia verrucosa (80 collections), Diderma alpinum (78) and Craterium leucocephalum (59) were the most consistently abundant myxomycetes. Other species represented by ≥15 collections were Didymium cf. dubium, Collaria lurida, Lamproderma arcyrioides and Didymium macquariense. The latter is a species new to science that was described from material collected during the present study. All of the species of myxomycetes now known to occur on Macquarie Island are members of the Trichiales, Physarales, Stemonitales or Echinosteliales; no member of the Liceales or Ceratiomyxales was ever collected.
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ZHURBENKO, Mikhail P., and Uwe BRAUN. "Cecidiomyces, a new subantarctic lichenicolous hyphomycete genus." Lichenologist 44, no. 6 (October 8, 2012): 801–6. http://dx.doi.org/10.1017/s0024282912000527.

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AbstractCecidiomyces santessonii gen. & sp. nov., found on Stereocaulon species on the subantarctic Macquarie Island (Tasmania, Australia), is described, illustrated and compared with other morphologically similar genera and species. It is characterized by a lichenicolous habit, gall-formation, caespitose to sporodochial colonies, semi-macronematous, monoblastic, determinate conidiophores reduced to conidiogenous cells, solitary, 0–1-euseptate, pigmented conidia, and schizolytic conidial secession.
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5

Smith, J. M. B., and T. P. Bayliss-Smith. "Kelp-plucking: coastal erosion facilitated by bull-kelp Durvillaea antarctica at subantarctic Macquarie Island." Antarctic Science 10, no. 4 (December 1998): 431–38. http://dx.doi.org/10.1017/s0954102098000522.

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Erosion of bedrock from lower intertidal reefs by waves acting on attached plants of bull-kelp (Durvillaea antarctica) was investigated over one year at Macquarie Island, Southern Ocean. At a site on the more sheltered east coast, such erosion occurred during four separate storms, each casting up 834–1078 large kelp plants km−1 of coast, of which 30–45% were still attached to jagged, freshly quarried bedrock fragments over 2.5 cm long. The largest fragment weighed was 74.6 kg; rounded cobbles and boulders attached to kelp plants and weighing up to 102.2 kg (and probably more than 160 kg) were also cast up on beaches. 19–21% of the standing crop of large kelp plants was removed by storms during the year of observation. Break points for 10 kelp stipes were found to be at least 90–161 kg. Total annual erosion by kelp-plucking is at least 1.56 tonnes of rock km−1 of coast. However, in terms of erosion this computes to only 0.1 mm yr−1, far below the rate of uplift of the island.
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6

Shaughnessy, Peter D., Catherine M. Kemper, and John K. Ling. "Records of vagrant phocid seals (family Phocidae) in South Australia." Australian Mammalogy 34, no. 2 (2012): 155. http://dx.doi.org/10.1071/am11036.

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Five species of phocid seal of the Southern Ocean and Antarctica come ashore occasionally on the southern Australian coast but do not breed there. We document records (specimens and sightings) of visits to South Australia (SA) by southern phocids from 1883 until August 2011. We used records from the SA Museum, reports from coastal officers of SA Department of Environment and Natural Resources (DENR), the DENR fauna database, information from the public, the literature and newspapers. Thirty-six southern elephant seal records included two births, in November 1932 and October 1986. The latter pup suckled for 20 days and then stayed ashore for eight weeks; both are similar to average durations at Macquarie Island. Of 33 dated records, 31 were between August and April, when elephant seals at Macquarie Island (the closest breeding site) are ashore to breed or moult. A recognisable male on Kangaroo Island has been sighted often over 10 years to 2010. Of the ice-breeding species, there were 54 leopard seal records. All of 40 dated records were between June and December, with the maximum (12) in August, similar to the seasonal distribution in Tasmania. There were five records of crabeater seals, one of a Ross seal, and one of a Weddell seal.
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7

KANTVILAS, Gintaras. "The genus Menegazzia (Lecanorales: Parmeliaceae) in Tasmania revisited." Lichenologist 44, no. 2 (February 8, 2012): 189–246. http://dx.doi.org/10.1017/s0024282911000685.

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AbstractWith 30 species, Tasmania is a major area of species diversity in the genus Menegazzia. Seven of these are new to science: M. abscondita Kantvilas, known from Tasmania and New Zealand, and M. athrotaxidis Kantvilas, M. hypogymnioides Kantvilas, M. petraea Kantvilas, M. ramulicola Kantvilas, M. subtestacea Kantvilas and M. tarkinea Kantvilas, all endemic to Tasmania. An identification key, descriptions based exclusively on Tasmanian collections, and detailed discussion of distribution, ecology, chemical composition and inter-species relationships are provided. All literature records of Menegazzia species pertaining to Tasmania are accounted for. New synonyms include: Menegazzia prototypica P. James and Parmelia pertusa var. coskinodes F. Wilson [synonyms of M. myriotrema (Müll. Arg.) R. Sant.], M. fertilis P. James [a synonym of M. platytrema (Müll. Arg.) R. Sant.] and Parmelia pertusa var. montana F. Wilson (a synonym of M. subtestacea). Incorrectly recorded species that should be deleted from the Tasmanian census include M. castanea P. James & D. J. Galloway (present on Macquarie Island) and M. testacea P. James & D. J. Galloway (endemic to New Zealand). The South American species, M. sanguinascens (Räs.) R. Sant., is recorded in Australasia (Tasmania) for the first time, whereas the widespread south-eastern Australian M. norstictica P. James is recorded for Western Australia. Salient features of the genus are discussed, including morphology, anatomy and chemistry. The biogeography of the genus is explored briefly. Twelve species (40%) are endemic to Tasmania, a level of endemism unmatched by any other species-rich genus on the island. Twelve species are shared with mainland Australia, eleven are shared with New Zealand, and only four species are shared with southern South America, all of which are sorediate, suggesting they are products of long-distance dispersal.
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8

Selkirk, J. M., and L. J. Saffigna. "Wind and Water Erosion of a Peat and Sand Area on Subantarctic Macquarie Island." Arctic, Antarctic, and Alpine Research 31, no. 4 (November 1999): 412. http://dx.doi.org/10.2307/1552590.

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9

Selkirk, J. M., and L. J. Saffigna. "Wind and Water Erosion of a Peat and Sand Area on Subantarctic Macquarie Island." Arctic, Antarctic, and Alpine Research 31, no. 4 (November 1999): 412–20. http://dx.doi.org/10.1080/15230430.1999.12003326.

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10

Orchard.A.E. "A revision of the Coprosma pumila (Rubiaceae) complex in Australia, New Zealand and the Subantarctic Islands." Brunonia 9, no. 2 (1986): 119. http://dx.doi.org/10.1071/bru9860119.

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The widespread complex of mat-forming Coprosma species, hitherto known as 'Coprosma pumila', plus some close allies (C. petriei, C. atropurpurea, C. nivalis) have been reexamined. C. pumila s. str. is shown to be restricted to the northern central plateau and Ben Lomond areas of Tasmania. The name C. perpusilla Col. is resurrected for the orange-fruited plants of Australia and New Zealand formerly included in C. pumila. A new subspecies, C. perpusilla ssp. subantarctica, is erected for the plants on Macquarie, Auckland, Camp- bell and Antipodes Islands. A new species, C. niphophila, is recognised for the Mt Kosciusko region and the South Island of New Zealand. The six species and two subspecies of the complex are keyed, fully described and illustrated, and their interrelation- ships, particularly their trans-Tasman vicariance, are discussed.
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Books on the topic "Erosion – Tasmania – Macquarie Island"

1

D, Seppelt R., and Selkirk D. R, eds. Subantarctic Macquarie Island: Environment and biology. Cambridge [England]: Cambridge University Press, 1990.

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2

Selkirk, Patricia, Rod Seppelt, and David Selkirk. Subantarctic Macquarie Island: Environment and Biology. Cambridge University Press, 2008.

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3

Stoney, Henry Butler. Residence in Tasmania: With a Descriptive Tour Through the Island, from Macquarie Harbour to Circular Head. Creative Media Partners, LLC, 2018.

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