Zooplankton Abundance in Australasian Waters

1962 ◽  
Vol 13 (2) ◽  
pp. 106 ◽  
Author(s):  
DJ Tranter

The seas surrounding Australia contain a relatively low zooplankton biomass, particularly in the open ocean. There is a region of higher biomass in an upwelling area between the north-west coast of Australia and Indonesia, and there are indications that there may be a shortlived spring increase in the southern Tasman Sea; otherwise, the biomass of zooplankton in the open ocean is no higher than in the Sargasso Sea. An examination of values for other parts of the world reveals that subtropical regions of the open ocean are characteristically poor in plankton. The mean zooplankton biomass on the Australian continental shelf was estimated to be about 100 mg/m³ (exclusive of salp swarms), varying from 82 to 213 mg/m³ with the area and the year. The biomass in the upwelling area south of Java was of the same magnitude, but in most parts of the open ocean it was no greatsr than 50 mg/m³, and was usually less than 25 mg/m³. Salp swarms were found more commonly in the southern part of the area investigated, and constituted local concentrations of higher biomass. These swarms took place in sprlng and summer and led to a seasonal cycle in the biomass level on the shelf regions of the New South Wales south coast. An increased biomass was also observed off the north-west coast of Australia during the period of prevailing offshore winds. This was crustacean in character.

2005 ◽  
Vol 84 (2) ◽  
pp. 149-165 ◽  
Author(s):  
Martin Rorke

This paper uses customs figures to show that herring exports from the east and west coast lowlands expanded significantly in the last six decades of the sixteenth century. The paper argues that the rise was primarily due to the north-west Highland fisheries being opened up and exploited by east and west coast burghs. These ventures required greater capital supplies and more complex organisation than their local inshore fisheries and they were often interrupted by political hostilities. However, the costs were a fraction of those required to establish a deepwater buss fleet, enabling Scotland to expand production and take advantage of European demand for fish while minimising additional capital costs.


2021 ◽  
Vol 3 (7) ◽  
Author(s):  
Otman EL Mountassir ◽  
Mohammed Bahir ◽  
Driss Ouazar ◽  
Abdelghani Chehbouni ◽  
Paula M. Carreira

AbstractThe city of Essaouira is located along the north-west coast of Morocco, where groundwater is the main source of drinking, domestic and agricultural water. In recent decades, the salinity of groundwater has increased, which is why geochemical techniques and environmental isotopes have been used to determine the main sources of groundwater recharge and salinization. The hydrochemical study shows that for the years 1995, 2007, 2016 and 2019, the chemical composition of groundwater in the study area consists of HCO3–Ca–Mg, Cl–Ca–Mg, SO4–Ca and Cl–Na chemical facies. The results show that from 1995 to 2019, electrical conductivity increased and that could be explained by a decrease in annual rainfall in relation to climate change and water–rock interaction processes. Geochemical and environmental isotope data show that the main geochemical mechanisms controlling the hydrochemical evolution of groundwater in the Cenomanian–Turonian aquifer are the water–rock interaction and the cation exchange process. The diagram of δ2H = 8 * δ18O + 10 shows that the isotopic contents are close or above to the Global Meteoric Water Line, which suggests that the aquifer is recharged by precipitation of Atlantic origin. In conclusion, groundwater withdrawal should be well controlled to prevent groundwater salinization and further intrusion of seawater due to the lack of annual groundwater recharge in the Essaouira region.


1851 ◽  
Vol 2 ◽  
pp. 239-240
Author(s):  
Thomas Anderson

About thirty years ago a species of manna, obtained from the Eucalyptus Mannifera, was brought from New South Wales, and was examined by Dr Thomas Thomson, and afterwards by Professor Johnston, both of whom ascertained it to contain a new species of sugar, different from the mannite which exists in ordinary manna. The author had, through the kindness of Mr Sheriff Cay, an opportunity of examining a very different species of manna, remarkable both from its chemical constitution, and from its possessing a definitely organised structure. This substance was discovered by Mr Robert Cay in 1844, in the interior of Australia Felix, to the north and north-west of Melbourne, where it occurs at certain seasons on the leaves of the Mallee plant, Eucalyptus Dumosa, and is known to the natives by the name of Lerp.


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