The distribution of red, yellow and grey earths in the Torrens Creek area, central north Queensland

Soil Research ◽  
1982 ◽  
Vol 20 (1) ◽  
pp. 1 ◽  
Author(s):  
RJ Coventry

Red, yellow, and grey earths mantle extensive plains in northern Australia. They have been studied in a semiarid, tropical area at Torrens Creek, some 200-300 km south-west of Townsville, Queensland. An examination of boreholes drilled along transects across these soils shows that the red earths usually occupy the lower slope sites and broad, non-channeled, drainage lines. The yellow and grey earths generally occur at midslope sites or over broadly convex upper regions of the low undulations that rise 10-30 m above the non-dissected parts of the plains. The distribution patterns of the red, yellow, and grey earths cannot be explained by differential weathering of the gently dipping Mesozoic sedimentary rock substrates. Nor can they be attributed to simple, topography-controlled, hydrological regimes in the soils. The distribution patterns of the different soils depend on factors related to the geology and the late Cainozoic geomorphic history of the area. These include the transported or sedentary nature of the soil parent materials, the hydrological regimes of the soils and of the weathered rock substrates, and the depth to the underlying, weathered rock.

Zoosymposia ◽  
2009 ◽  
Vol 2 (1) ◽  
pp. 537-550
Author(s):  
SHONA A. HOCKNULL ◽  
CHRISTOPHER J. GLASBY

This study identifies to species or species units 572 lots (>1000 specimens) of pilargids from six localities in the Arafura Sea and Gulf of Carpentaria (including the ports at Gove and McArthur River). We analyze the taxonomic data against geomorphic unit, depth, and sediment type. Preliminary results show that pilargid fauna of northern Australia comprises 13 species in seven genera (Ancistrosyllis, Cabira, Litocorsa, Loandalia, Pilargis, Sigambra, and Synelmis). Although all four localities have a similar diversity of species (six or seven species each), the species composition differs between each region: Litocorsa annamita and Synelmis rigida were found in all sediment types in the Arafura Sea and Gulf of Carpentaria; Ancistrosyllis cf. hartmanae (mud and sand dominated sediments only) and Sigambra pettiboneae (all sediment types) were restricted to the inshore localities of Gove and McArthur River; Loandalia gladstonensis and Sigambra sp. 2 were found on the shelf and in the inshore habitats of the Gulf of Carpentaria only; Litocorsa sp. ‘arafura’, Sigambra sp. ‘arafura’ and Synelmis gibbsi were found only in the Arafura Sea, with sediments dominated by sand and gravel; and Cabira sp. 1 and Sigambra cf. tentaculata were found at all locations, in all sediment types. Based on these distribution patterns and the Recent Quaternary geological history of the area, hypotheses of post-glacial colonization of the Gulf of Carpentaria are presented. The pilargid species composition in northern Australia is also compared to neighboring Indo-west Pacific regions.


Zootaxa ◽  
2021 ◽  
Vol 5068 (4) ◽  
pp. 547-571
Author(s):  
IAN SMALES

Uncertainty about taxonomy and nomenclature of the Australian long-necked turtle Chelodina oblonga has ensued since its description by Gray in 1841. This has been due to the general nature of information about provenance of the lectotype specimen and the ostensible morphological similarity of the specimen to another taxon from northern Australia that confused Gray and many subsequent workers. The south-western Australian provenance of the specimen has recently been confirmed by Shea et al. (2020). The present paper provides a detailed consideration of morphology of the specimen and compares it with other specimens available to Gray and to larger series that are now available. The study elucidates morphological aspects that have underlain the history of confusion and it highlights a number of characters that consistently differentiate adults of the relevant taxa. These demonstrate that morphology of the C. oblonga lectotype conforms with the taxon from the south-west of Western Australia, as has also been confirmed by recently published investigations of mitogenomics and historical information about provenance of the lectotype.  


2020 ◽  
Vol 58 ◽  
pp. 118-134
Author(s):  
Aleksandr E. Kotov

The journal of Ksenofont A. Govorsky “Vestnik Yugo-Zapadnoy I Zapadnoy Rossii” (“South-West and West Russia Herald”) is known in the history of pubic thought as odious and reactionary. However, this stereotypical image needs some revision: the anti-Polish discourse on the pages of the magazine was not so much nationalistic as anti-aristocratic in nature. Considering the “Poles” primarily as carriers of the aristocratic principles, the editorial board of the magazine claimed to protect the broad masses of the people. Throughout its short history, the magazine consistently opposed both revolutionary and aristocratic propaganda. However, the regional limitations of the problems covered in the magazine did not give it the opportunity to reflect on the essential closeness of the revolutionary and reactionary principles. Yu.F. Samarin and I.S. Aksakov – whose conservative-democratic views, on the whole, were close to “Western Russianism”, promoted by the authors of “Vestnik Yugo-Zapadnoy I Zapadnoy Rossii”, managed to reach that goal.


2021 ◽  
Vol 21 (1) ◽  
pp. 28-52
Author(s):  
Sam Harper ◽  
Ian Waina ◽  
Ambrose Chalarimeri ◽  
Sven Ouzman ◽  
Martin Porr ◽  
...  

This paper explores identity and the recursive impacts of cross-cultural colonial encounters on individuals, cultural materials, and cultural practices in 20th-century northern Australia. We focus on an assemblage of cached metal objects and associated cultural materials that embody both Aboriginal tradition and innovation. These cultural materials were wrapped in paperbark and placed within a ring of stones, a bundling practice also seen in human burials in this region. This ‘cache' is located in close proximity to rockshelters with rich, superimposed Aboriginal rock art compositions. However, the cache shelter has no visible art, despite available wall space. The site shows the utilisation of metal objects as new raw materials that use traditional techniques to manufacture a ground edge metal axe and to sharpen metal rods into spears. We contextualise these objects and their hypothesised owner(s) within narratives of invasion/contact and the ensuing pastoral history of this region. Assemblage theory affords us an appropriate theoretical lens through which to bring people, places, objects, and time into conversation.


1928 ◽  
Vol 11 ◽  
pp. 83-115
Author(s):  
Gladys A. Thornton

Clare is situated in the south-west corner of Suffolk, in the valley of the Stour River. At the present day it is only a village, for its market is no longer held; yet its history shows that in earlier times it was of considerable importance, especially during the medieval period, when it was a favourite residence of the Clare lords. The town then had a busy market and a flourishing cloth-making industry; and at one time it seemed possible that Clare might attain full development as a borough, possessing as it did some burghal characteristics. In the following pages it is proposed to study in detail the history of Clare as a seignorial borough during the Middle Ages, and its subsequent development.


2019 ◽  
Vol 186 (4) ◽  
pp. 934-949 ◽  
Author(s):  
Danilo Harms ◽  
J Dale Roberts ◽  
Mark S Harvey

Abstract The south-western division of Australia is the only biodiversity hotspot in Australia and is well-known for extreme levels of local endemism. Climate change has been identified as a key threat for flora and fauna, but very few data are presently available to evaluate its impact on invertebrate fauna. Here, we derive a molecular phylogeography for pseudoscorpions of the genus Pseudotyrannochthonius that in the south-west are restricted to regions with the highest rainfall. A dated molecular phylogeny derived from six gene fragments is used for biogeographic reconstruction analyses, spatial mapping, environmental niche-modelling, and to infer putative species. Phylogenetic analyses uncover nine clades with mostly allopatric distributions and often small linear ranges between 0.5 and 130 km. Molecular dating suggests that the origins of contemporary diversity fall into a period of warm/humid Palaeogene climates, but splits in the phylogeny coincide with major environmental shifts, such as significant global cooling during the Middle Miocene. By testing several models of historical biogeography available for the south-west, we determine that Pseudotyrannochthonius is an ancient relict lineage that principally follows a model of allopatric speciation in mesic zone refugia, although there are derivations from this model in that some species are older and distribution patterns more complex than expected. Ecological niche models indicate that drier and warmer future climates will lead to range contraction towards refugia of highest rainfall, probably mimicking past variations that have generated high diversity in these areas. Their conservation management will be crucial for preserving the unique biodiversity heritage of the south-west.


2012 ◽  
Vol 31 (2) ◽  
pp. 268-274 ◽  
Author(s):  
Michael T. Hirschmann ◽  
Stephan Schön ◽  
Faik K. Afifi ◽  
Felix Amsler ◽  
Helmut Rasch ◽  
...  

1963 ◽  
Vol 58 ◽  
pp. 30-43 ◽  
Author(s):  
J. N. Coldstream

On the east slope of Lower Gypsades hill, about 100 metres west of the Temple Tomb, a chamber tomb came to light in August 1958, when a cutting for a new water pipe was driven through the area (A in Plate 9 a). In the course of this operation, part of a plain larnax (iii) was sliced off, and much earth removed from the west end of the collapsed chamber: at no point, however, had the municipal workmen penetrated to the tomb floor.The chamber was approached by a sloping dromos (Plate 9 a: length 2·80 metres; max. width 1 metre), roughly cut into the natural kouskouras rock: its walls were approximately perpendicular. Although the gradient varied a good deal, there was no suggestion of a stairway.The blocking wall was found in good condition. Of especial interest were the numerous fragments of larnakes that had been built into its fabric: some of them could be recognized as belonging to each of the three fragmentary larnakes (i, ii, v) whose scattered pieces were found below and around the two undisturbed burials in the chamber (iii, iv). We may thus distinguish two periods in the history of the tomb: larnakes i, ii, and v were evidently smashed up in order to make room for iv and iii, which must have been deposited in that order. The debris of v was found under iv, with a few adult bones in its wreckage. Part of i lay on the floor near the south-west corner, where two plain vases (2, 3) were found in situ, hence, also, came most of the fragments of the fine L.M. IIIA 2 stirrup vase (1), although its other pieces were scattered all over the floor of the tomb. This small group of offerings may belong to the disturbed adult skeleton, whose skull lay up against the lower edge of iii. Curiously, some fragments of i and ii were also found above the broken lid of iv (Plate 9 b): perhaps the lid of the later larnax was accidentally smashed at the time of the funeral, in which case the debris from earlier burials could have been piled up above it, as a rough and ready means of protection.


2017 ◽  
Vol 59 (2) ◽  
pp. 105
Author(s):  
N. DIAKAKIS (Ν.ΔΙΑΚΑΚΗΣ)

Enterolithiasis is characterized by the presence of enteroliths in the large colon of horses with the ascending colon being the most common site of obstruction. Enteroliths are composed of ammonium magnesium phosphate, which is supplied both by the digestive processes intestinal bacteria and by feeds. The enteroliths typically form around a central nidus. Although enterolithiasis is seen all over the world, the most cases are reported from North America, and more specifically, California, South West Indiana and Florida. As far as breed is concerned, it affects predominantly Arab horses and rarely Quarter and Thoroughbreds. As far as age is concerned, it is usually seen in middle-aged horses. Although the pathogenesis of enterolithiasis is not fully understood, nutrition and heritability are believed to be a part in it. A rich diet in ammonium, magnesium and phosphorus predisposes to enterolith formation, as those elements are the main components of enteroliths. Clinical signs vary considerably and are rarely characteristic of the disease. Usually, the presence of the enterolith is free of symptoms unless it leads to obstruction. In most cases of enterolithiasis a small amount of faeces, air and the administered mineral oil could pass from the obstruction site. On the contrary, in complete obstructions the passage is closed, defecation is absent and no laxative can pass the obstruction site. The enterolith is rarely found by rectal examination. A history of recurrent colic might be connected to the presence of enteroliths that cause partial or temporary obstruction. The most accurate method for diagnosing enterolithiasis is abdominal radiography. The treatment of choice is the surgical removal of enteroliths, which has a favorable prognosis provided that the laparotomy is going to take place early in course of the disease, before the onset of peritonitis. Intestinal rupture, which rapidly leads to peritonitis, is the gravest and commonest complication. Other complications are colitis, leakage through the laparotomy site and peritonitis. In order to prevent reformation of enteroliths, the daily consumption of alfalfa hay has to be reduced dramatically and poor quality hay has to be administered.


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