Isozymes, secondary compounds and experimental cultures of Australian seagrasses in Halophila, Halodule, Zostera, Amphibolis and Posidonia

1981 ◽  
Vol 29 (3) ◽  
pp. 247 ◽  
Author(s):  
C McMillan ◽  
SC Williams ◽  
L Escobar ◽  
O Zapata
Keyword(s):  
New South ◽  
New South Wales ◽  
South Australia ◽  
Leaf Size ◽  
Secondary Compounds ◽  
The Other ◽  
Enzyme Systems ◽  
South Wales ◽  
Ecological Implications

Systematic and ecological implications were shown for Australian seagrasses by studies of isozymes, secondary compounds and experimental cultures. In Halophila, small- and large-leaved plants which occur sympatrically from northern Queensland to New South Wales and were referred to H. ovalis (R.Br.) Hook. f. differed in isozymes and secondary compounds and maintained leaf size differences in experimental cultures. The small-leaved plants should be referred to a different species. In Halodule, narrow-leaved plants that were referred to H. uninervis (Forsk.) Aschers. and H.pinifolia (Miki) Den Hartog were examined. In experimental cultures, narrow-leaved plants from Thursday Island produced both tridentate and rounded serrulate leaf tips and differed in isozymes and secondary compounds from wide-leaved plants. The narrow- leaved plants should be referred to H. pinifolia and the wide-leaved plants to H. uninervis. In Zostera, small- and large-leaved forms of Z. capricorni Aschers. which occur sympatrically in Queensland and New South Wales have similar isozymes that differ from those of Z. muelleri Irmisch. ex Aschers. of South Australia. Experimental cultures of Z. capricorni continued to produce 5-nerved leaves and those of Z. muelleri, 3- nerved leaves. In Amphibolis, cultures of A. antarctica (Labill.) Sonder & Aschers. and A. griffithii (J. M. Black) Den Hartog continued to show leaf differences but were similar in secondary compounds and isozymes, differing in only one of eight enzyme systems. In Posidonia, wide-leaved plants of P. australis Hook. f. continued to produce leaves in culture that differed in width from those of P. sinuosa Cambridge & Kuo but were similar in secondary compounds and isozymes, differing only in one of eight enzyme systems. The chemical evaluations and experimental cultures suggested wide differences in Halophila and in Halodule but indicated only narrow differences in the other three genera.

scholarly journals Early Discoveries of the Effects of Ice Action in Australia

1987 ◽  
Vol 33 (114) ◽  
pp. 231-235
Author(s):  
Maxwell R. Banks ◽  
Eric A. Colhoun ◽  
David Hannan
Keyword(s):  
Great Britain ◽  
New South ◽  
New South Wales ◽  
South Australia ◽  
The Other ◽  
Macquarie Island ◽  
Late Palaeozoic ◽  
South Wales ◽  
Central Highlands ◽  
The One

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.

scholarly journals Early Discoveries of the Effects of Ice Action in Australia

1987 ◽  
Vol 33 (114) ◽  
pp. 231-235 ◽  
Author(s):  
Maxwell R. Banks ◽  
Eric A. Colhoun ◽  
David Hannan
Keyword(s):  
Great Britain ◽  
New South ◽  
New South Wales ◽  
South Australia ◽  
The Other ◽  
Macquarie Island ◽  
Late Palaeozoic ◽  
South Wales ◽  
Central Highlands ◽  
The One

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.

In A Fix: Fixed-Term Parliaments in the Australian States

2013 ◽  
Vol 41 (2) ◽  
pp. 265-298
Author(s):  
Peter Congdon
Keyword(s):  
Western Australia ◽  
Prime Minister ◽  
New South ◽  
New South Wales ◽  
South Australia ◽  
Constitutional Amendments ◽  
South Wales

Constitutional systems of Westminster heritage are increasingly moving towards fixed-term parliaments to, amongst other things, prevent the Premier or Prime Minister opportunistically calling a ‘snap election’. Amongst the Australian states, qualified fixed-term parliaments currently exist in New South Wales, South Australia and Victoria. Queensland, Tasmania and Western Australia have also deliberated over whether to establish similar fixed-term parliaments. However, manner and form provisions in those states' constitutions entrench the Parliament's duration, Governor's Office and dissolution power. In Western Australia and Queensland, unlike Tasmania, such provisions are doubly entrenched. This article considers whether these entrenching provisions present legal obstacles to constitutional amendments establishing fixed-term parliaments in those two states. This involves examining whether laws fixing parliamentary terms fall within section 6 of the Australia Acts 1986 (Cth) & (UK). The article concludes by examining recent amendments to the Electoral Act 1907 (WA) designed to enable fixed election dates in Western Australia without requiring a successful referendum.

The Relation Between the Food of the Australian Barracouta, Thyrsites atun (Euphrasen), and Recent Fluctuations in the Fisheries

1957 ◽  
Vol 8 (1) ◽  
pp. 29 ◽  
Author(s):  
M Blackburn
Keyword(s):  
Population Distribution ◽  
New South ◽  
New South Wales ◽  
South Australia ◽  
Downward Trend ◽  
Small Fish ◽  
Fish Diet ◽  
Upward Trend ◽  
Independent Evidence ◽  
South Wales

The diet of surface-swimming Australian barracouta was studied from over 10,000 stomachs. The principal prey organisms in Bass Strait are the euphausiid Nyctiphanes australis Sars, the anchovy Engraulis australis (White), and young barracouta, in that order; and in eastern Tasmania Nyctiphanes, Engraulis, and the sprat Clupea bassensis McCulloch, in that order. The pilchard Sardinops neopilchardus (Steindachner) is not an important item of the diet in these regions although it is so in New South Wales, South Australia, and Western Australia. The jack mackerel Trachurus declivis Jenyns is a significant item in eastern Tasmania and New South Wales but not in Bass Strait. These and other features of the fish diet of the barracouta reflect actual availability of the various small fish species in the waters. Barracouta eat Nyctiphanes by herding them into dense masses (or finding them already concentrated) and swallowing them. The movements of the anchovy make it unavailable to Bass Strait and eastern Tasmanian barracouta for much of the summer and autumn period, when the barracouta are thus dependent upon Nyctiphanes for the bulk of their food. A close positive relationship between the availability of barracouta and Nyctiphanes might therefore be expected at those seasons. There is evidence of such a relationship between mean availability (catch per boat-month) of barracouta and mean percentage of barracouta stomachs containing Nyctiphanes, at those seasons, from year to year. For southern Victorian coastal waters both show a downward trend from 1948-49 to 1950-51 and then an upward trend to 1953-54; for eastern Tasmania both show a downward trend (for autumn only) from 1949-50 through 1952-53. The records of catch per boat-month furnish independent evidence that the main variations in this index were effects of availability (population distribution or behaviour) rather than abundance (population size), at least for southern Victoria. It is therefore considered that when scarcity of barracouta occurs in summer and autumn in the coastal fishing areas it may be due to scarcity of Nyctiphanes, forcing the fish to go offshore for this food which is known to be available there. This would take the fish out of range of the fishermen.

Dacus tryoni. [Distribution map].

1960 ◽  
Author(s):  
Keyword(s):  
Geographical Distribution ◽  
New South ◽  
New South Wales ◽  
South Australia ◽  
Fruit Fly ◽  
Distribution Map ◽  
Bactrocera Tryoni ◽  
South Wales ◽  
New Distribution

Abstract A new distribution map is provided for Dacus tryoni[Bactrocera tryoni] (Frogg.) (Dipt., Trypetidae) (Queensland Fruit-fly) Hosts: Many deciduous and subtropical fruits. Information is given on the geographical distribution in AUSTRALIA, New South Wales, Queensland, South Australia, Victoria.

Podospora excentrica. [Descriptions of Fungi and Bacteria].

2020 ◽  
Author(s):  
D. W. Minter
Keyword(s):  
New Zealand ◽  
South America ◽  
Atlantic Ocean ◽  
Geographical Distribution ◽  
Western Australia ◽  
New South ◽  
Conservation Status ◽  
New South Wales ◽  
South Australia ◽  
South Wales

Abstract A description is provided for Podospora excentrica. Some information on its associated organisms and substrata, dispersal and transmission, habitats and conservation status is given, along with details of its geographical distribution (South America (Venezuela), Atlantic Ocean (Portugal (Madeira)), Australasia (Australia (New South Wales, South Australia, Victoria, Western Australia)), New Zealand, Europe (Belgium, Denmark, Germany, Ireland, Italy, Netherlands, Spain, Sweden, UK)).

John Davies Thomas: Chloroformist in London and pioneer South Australian doctor

2021 ◽  
pp. 0310057X2110315
Author(s):  
Rajesh P Haridas
Keyword(s):  
Medical Journal ◽  
North America ◽  
New South ◽  
New South Wales ◽  
Medical Officer ◽  
South Australia ◽  
Adelaide Hospital ◽  
Medical Society ◽  
College Hospital ◽  
South Wales

John Davies Thomas (1844–1893) described a two-ounce drop-bottle for chloroform in 1872 while he was a resident medical officer at University College Hospital, London. After working as a ship’s surgeon, he settled in Australia. In May 1875, Thomas presented a paper on the mortality from ether and chloroform at a meeting of the Medical Society of Victoria in Melbourne, Victoria. Surveys conducted in Europe and North America had established that the mortality from chloroform was eight to ten times higher than that from ether. At that time, chloroform was the most widely administered anaesthetic in Australia. Thomas’ paper was published in The Australian Medical Journal and reprinted by the Medical Society of Victoria for distribution to hospitals in the Colony of Victoria. Later that year, Thomas moved to Adelaide, South Australia, where he may have been influential at the Adelaide Hospital in ensuring that ether was administered more often than chloroform. It does not appear that Thomas’ papers on anaesthesia had a significant effect on the conduct of anaesthesia in Victoria or New South Wales.

Sign in / Sign up

Export Citation Format

Share Document