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Journal articles on the topic 'Glenelg'

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Published: 4 June 2021

Last updated: 7 February 2022

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1

Rawson, J. R., D. A. Carswell, and D. Smallwood. "Garnet-bearing olivine-websterite within the Eastern Glenelg Lewisian of the Glenelg Inlier, NW Highlands." Scottish Journal of Geology 37, no. 1 (May 2001): 27–34. http://dx.doi.org/10.1144/sjg37010027.

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2

Anderson, J. A. C., and C. M. Gray. "Geological affinities of the Glenelg river complex, western Victoria." Australian Journal of Earth Sciences 41, no. 2 (April 1994): 141–55. http://dx.doi.org/10.1080/08120099408728122.

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3

Ii, Hiroyuki, John Sherwood, and Nick Turoczy. "Salinization of the Glenelg River in Southwest Victoria, Australia." SIL Proceedings, 1922-2010 30, no. 10 (April 2010): 1515–19. http://dx.doi.org/10.1080/03680770.2009.11902367.

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4

STRACHAN, R. A., and P. J. TRELOAR. "A Grenville Sm/Nd age for the Glenelg eclogite." Nature 314, no. 6013 (April 1985): 754. http://dx.doi.org/10.1038/314754a0.

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5

SANDERS, I. S. "A Grenville Sm/Nd age for the Glenelg eclogite (reply)." Nature 314, no. 6013 (April 1985): 754–55. http://dx.doi.org/10.1038/314754b0.

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6

Lind, P. R., B. J. Robson, B. D. Mitchell, and T. G. Matthews. "Can sand slugs in rivers deliver conservation benefits? The biodiversity value of tributary junction plug wetlands in the Glenelg River, Australia." Marine and Freshwater Research 60, no. 5 (2009): 426. http://dx.doi.org/10.1071/mf08175.

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Restoration works are carried out to alleviate human impacts and improve habitats within ecosystems. However, human impacts may also create new (anthropogenic) habitat for species to exploit. A dilemma arises when proposed restoration works would remove anthropogenic habitat and the assemblages it supports. Sediment input into the Glenelg River has formed tributary junction plug wetlands at confluences. Sand slug removal is proposed as part of river rehabilitation, but would also drain plug wetlands. We sampled four plug wetland, four river run and three river pool sites to determine whether plug wetlands influence water quality and add to the biodiversity of macroinvertebrates in the Glenelg River. Water quality and macroinvertebrate diversity were similar in plug wetlands, river runs and river pools. Assemblages were distinct among all sites, regardless of type, so there was no characteristic ‘plug-wetland fauna’. Therefore, although removal of plug wetlands would not cause a dramatic loss of invertebrate biodiversity, it would destroy anthropogenic habitat that supports a similar range of species to natural habitats in a river subject to multiple degrading processes. Gains from rehabilitation should be weighed against the value of anthropogenic habitat and the extent of similar habitat lost elsewhere in the ecosystem.

7

Irving, A. D., K. F. Raphael, P. M. Rennison, R. Lewis, C. D. Cruickshank, and R. A. Rengifo. "The Elgin, Franklin, Glenelg and West Franklin fields, Blocks 22/30b, 22/30c, 29/4d, 29/5b and 29/5c, UK North Sea." Geological Society, London, Memoirs 52, no. 1 (2020): 436–46. http://dx.doi.org/10.1144/m52-2018-47.

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AbstractThe Elgin, Franklin, Glenelg and West Franklin fields lie approximately 240 km (150 miles) east of Aberdeen in Blocks 22/30b, 22/30c, 29/4d, 29/5b and 29/5c of the UK Central Graben. Franklin was discovered in 1985, Elgin in 1991, Glenelg in 1999 and West Franklin in 2003. Elgin is a complex faulted anticline comprising four panels, while the others are simpler, tilted fault block structures. The main reservoir is the Upper Jurassic Fulmar Formation shoreface sandstone, although the Middle Jurassic Pentland and Triassic Skagerrak formations have also been produced on Franklin. Initial pressure was c. 1100 bar (16 000 psi), with a reservoir temperature of around 190°C (375°F). Production wells are drilled from four wellhead platforms; all connected to a central process, utilities and quarters facility above Elgin. Gas and condensate production started in 2001 from six wells on each of Elgin and Franklin, with the plateau being extended by satellite and infill wells. The project remains the world's largest high-pressure–high-temperature development, requiring continued innovations in geoscience, drilling, completion and operations. Cumulative production at end 2017 is 886 Mboe, with estimated ultimate recovery around 1300 Mboe.

8

Davis, Wendy. "The End of an Era: Sixteen Years of the Adelaide Theological Library." ANZTLA EJournal, no. 12 (May 20, 2015): 2–6. http://dx.doi.org/10.31046/anztla.vi12.278.

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Presented at the End of an Era dinner held 12th November, 2013 at the Glenelg Golf Club. The dinner marks the departure of Catholic Theological College from the Adelaide College of Divinity. Catholic Theological College ceases to exist from 2014. Catholic postgraduate students will continue their studies through the Australian Catholic University, and most staff of CTC will become part of the ACU faculty.

9

Turner, S. P., C. J. Adams, T. Flöttmann, and J. D. Foden. "Geochemical and geochronological constraints on the Glenelg River Complex, western Victoria." Australian Journal of Earth Sciences 40, no. 3 (June 1993): 275–92. http://dx.doi.org/10.1080/08120099308728080.

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10

Nicholson, Geoff, Gregory P. Jenkins, John Sherwood, and Andy Longmore. "Physical environmental conditions, spawning and early-life stages of an estuarine fish: climate change implications for recruitment in intermittently open estuaries." Marine and Freshwater Research 59, no. 8 (2008): 735. http://dx.doi.org/10.1071/mf07197.

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Significant variation in the egg and larval survival and juvenile recruitment of estuarine fishes has been linked to fluctuating environmental conditions. This present study compared the distribution and abundance of black bream (Acanthopagrus butcheri) eggs and yolk-sac larvae between two microtidal estuaries of different flow regimes, where the riverine flow into the Glenelg estuary was around eight times the flow volume into the Hopkins estuary. Samples were collected monthly from September to November at sites along each estuary where vertical profiles of temperature, salinity and dissolved oxygen (DO) were measured, and vertically stratified sampling of black bream eggs and yolk-sac larvae was conducted using a Schindler sampler. Salt wedge formation was apparent in both estuaries, with significant de-oxygenation of deeper, saline waters. Eggs occurred in a wide range of DO levels but yolk-sac larvae were less common at the lowest levels. Most eggs and yolk-sac larvae were collected in salinities greater than 10. Results suggested that egg mortality was higher in the Hopkins than the Glenelg estuary, which may be associated with the hypoxic conditions characteristic of low-flow conditions. The results have significant implications in terms of climate change that is predicted to lead to warmer, drier conditions in south-eastern Australia, potentially increasing stratification and subsequent hypoxic zones.

11

STOREY, C. D., T. S. BREWER, and S. TEMPERLEY. "P–T conditions of Grenville-age eclogite facies metamorphism and amphibolite facies retrogression of the Glenelg–Attadale Inlier, NW Scotland." Geological Magazine 142, no. 5 (September 2005): 605–15. http://dx.doi.org/10.1017/s001675680500110x.

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Peak and retrograde P–T conditions of Grenville-age eclogites from the Glenelg–Attadale Inlier of the northwest Highlands of Scotland are presented. Peak conditions are estimated as c. 20 kbar and 750–780°C, in broad agreement with previous work. The eclogites subsequently followed a steep decompression path to c. 13 kbar and 650–700°C during amphibolite facies retrogression. Peak eclogite facies metamorphism occurred > 1080 Ma and retrogression at c. 995 Ma, suggesting fairly sluggish uplift rates of < 0.3 km/Ma and cooling rates of < 1.25°C/Ma, when compared with other parts of the Grenville orogeny and/or modern orogens. However, current poor constraints on the timing of peak metamorphism mean that these rates cannot be used to interpret the geodynamic evolution of this part of the orogen. The P–T–t data, together with petrology and the field relationships between the basement rocks of the Glenelg–Attadale Inlier and the overlying Moine Supergroup, mean that it is difficult to support the currently held view that an unconformable relationship exists between the two. It is suggested that more data are required in order to re-interpret the Neoproterozic tectonic evolution of the northwest Highlands of Scotland.

12

Kemp, A. I. S., C. M. Gray, D. J. Ellis, J. A. C. Anderson, and D. J. Ferguson. "Delamerian Glenelg tectonic zone, western Victoria: Characterisation and synthesis of igneous rocks." Australian Journal of Earth Sciences 49, no. 2 (April 2002): 201–24. http://dx.doi.org/10.1046/j.1440-0952.2002.00920.x.

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13

Gray, C. M., A. I. S. Kemp, J. A. C. Anderson, D. J. Bushell, D. J. Ferguson, J. Fitzherbert, and M. D. Stevenson. "Delamerian Glenelg tectonic zone, western Victoria: Geology and metamorphism of stratiform rocks." Australian Journal of Earth Sciences 49, no. 2 (April 2002): 187–200. http://dx.doi.org/10.1046/j.1440-0952.2002.00922.x.

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14

Brewer, T. S., C. D. Storey, R. R. Parrish, S. Temperley, and B. F. Windley. "Grenvillian age decompression of eclogites in the Glenelg–Attadale Inlier, NW Scotland." Journal of the Geological Society 160, no. 4 (July 2003): 565–74. http://dx.doi.org/10.1144/0016-764902-061.

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15

Playford, Timothy J., and Keith F. Walker. "Status of the endangered Glenelg River Mussel Hyridella glenelgensis (Unionoida: Hyriidae) in Australia." Aquatic Conservation: Marine and Freshwater Ecosystems 18, no. 5 (October 17, 2007): 679–91. http://dx.doi.org/10.1002/aqc.877.

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16

Sanders, I. S. "Plagioclase breakdown and regeneration reactions in Grenville kyanite eclogite at Glenelg, NW Scotland." Contributions to Mineralogy and Petrology 98, no. 1 (January 1988): 33–39. http://dx.doi.org/10.1007/bf00371907.

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17

Sajeev, Krishnan, Takahiro Kawai, Soichi Omori, Brian F. Windley, and Shigenori Maruyama. "P–T evolution of Glenelg eclogites, NW Scotland: Did they experience ultrahigh-pressure metamorphism?" Lithos 114, no. 3-4 (February 2010): 473–89. http://dx.doi.org/10.1016/j.lithos.2009.10.007.

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18

Sanders, I. S. "Phase relations and P-T conditions for eclogite-facies rocks at Glenelg, north-west Scotland." Geological Society, London, Special Publications 43, no. 1 (1989): 513–17. http://dx.doi.org/10.1144/gsl.sp.1989.043.01.49.

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19

Kemp, A. I. S., and C. M. Gray. "Geological context of crustal anatexis and granitic magmatism in the northeastern Glenelg River Complex, western Victoria." Australian Journal of Earth Sciences 46, no. 3 (June 1999): 407–20. http://dx.doi.org/10.1046/j.1440-0952.1999.00714.x.

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20

Barber, A. J. "The structure of the Glenelg-Attadale Lewisianoid Inlier and its relationship to the Moine Thrust Zone." Scottish Journal of Geology 47, no. 2 (November 2011): 113–32. http://dx.doi.org/10.1144/0036-9276/01-427.

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21

Miller, AD, OF Sweeney, NS Whiterod, AR Van Rooyen, M. Hammer, and AR Weeks. "Critically low levels of genetic diversity in fragmented populations of the endangered Glenelg spiny freshwater crayfish Euastacus bispinosus." Endangered Species Research 25, no. 1 (July 31, 2014): 43–55. http://dx.doi.org/10.3354/esr00609.

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22

Gibson, G. M., and D. N. Nihill. "Glenelg River Complex: Western margin of the Lachlan Fold Belt or extension of the Delamerian Orogen into Western Victoria?" Tectonophysics 214, no. 1-4 (November 1992): 69–91. http://dx.doi.org/10.1016/0040-1951(92)90191-8.

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23

Hammer, Michael P., Mark Adams, Peter J. Unmack, and Keith F. Walker. "A rethink on Retropinna: conservation implications of new taxa and significant genetic sub-structure in Australian smelts (Pisces:Retropinnidae)." Marine and Freshwater Research 58, no. 4 (2007): 327. http://dx.doi.org/10.1071/mf05258.

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The smelt genus Retropinna nominally includes three small (<150 mm) freshwater fish species endemic to south-eastern Australia and New Zealand. For the two Australian species, the broad range of R. semoni (Weber) on the mainland suggests some vulnerability to isolation and genetic divergence, whereas the apparent confinement of R. tasmanica McCulloch to Tasmania is curious if, as suspected, it is anadromous. Analyses of Australian material using allozyme electrophoresis show five genetically distinct species with contiguous ranges and no evidence of genetic exchange. Three occur along the eastern seaboard (including three instances of sympatry), another in coastal and inland south-eastern Australia and Tasmania, and a fifth species in the Lake Eyre Basin. There is no indication of a simple ‘tasmanica’ v. ‘semoni’ dichotomy, but instead a complex pattern involving discrete clusters for the Upper Murray plus Darling rivers, Lower Murray, Glenelg River and Tasmanian regions, with coastal western Victorian samples having varying affinity to these groups. The overall pattern is one of deep divergences among species and strong genetic sub-structuring within and provides a strong argument for extended studies to prepare for appropriate conservation measures.

24

Strachan, R. A., T. E. Johnson, C. L. Kirkland, P. D. Kinny, and T. Kusky. "A Baltic heritage in Scotland: Basement terrane transfer during the Grenvillian orogeny." Geology 48, no. 11 (July 21, 2020): 1094–98. http://dx.doi.org/10.1130/g47615.1.

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Abstract Archean basement inliers within the Northern Highland terrane (NHT), Scottish Caledonides, have been correlated with the Lewisian Gneiss Complex of the Laurentian foreland. New zircon U-Pb ages indicate that the NHT basement contains evidence for magmatism at 2823–2687 Ma and 1772–1655 Ma. The first group compares with crystallization ages of the foreland Archean gneisses. However, the second group, and a supracrustal unit, formed ∼100–250 m.y. after the youngest major phase of juvenile magmatism and sedimentation in the foreland. Also, there is no indication within the NHT basement of the Paleoproterozoic mafic and felsic intrusions common within the foreland, leading us to conclude that there is no firm basis for correlation of the two crustal blocks. The Caledonian Moine thrust, which separates the foreland and the NHT basement, is thought to have reworked a Grenvillian suture indicated by the presence of the ca. 1100–1000 Ma Eastern Glenelg eclogites. On the basis of the new isotopic data, we propose that the NHT basement was a fragment of Baltica that was emplaced onto Laurentia during the Grenvillian orogeny, representing a further example of basement terrane transfer in the circum–North Atlantic orogens.

25

SUITER, J., R. ROMANI, J. ARNAUD, S. HOLLINGWORTH, and K. HAWKINS. "Reducing structural uncertainties through anisotropic pre-stack depth imaging: examples from the Elgin/Franklin/Glenelg HP/HT fields area, Central North Sea." Geological Society, London, Petroleum Geology Conference series 6, no. 1 (2005): 1435–48. http://dx.doi.org/10.1144/0061435.

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26

Storey, Craig. "The Glenelg-Attadale Inlier, NW Scotland, with emphasis on the Precambrian high-pressure metamorphic history and subsequent retrogression: an introduction and review." Scottish Journal of Geology 44, no. 1 (April 2008): 1–16. http://dx.doi.org/10.1144/sjg44010001.

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27

Storey, Craig. "A field guide to the Glenelg-Attadale Inlier, NW Scotland, with emphasis on the Precambrian high-pressure metamorphic history and subsequent retrogression." Scottish Journal of Geology 44, no. 1 (April 2008): 17–34. http://dx.doi.org/10.1144/sjg44010017.

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28

Grixti, Daniel, Simon D. Conron, Alexander Morison, and Paul L. Jones. "Estimating post-release survival and the influential factors for recreationally caught Black bream (Acanthopagrus butcheri) in the Glenelg River, south eastern Australia." Fisheries Research 92, no. 2-3 (August 2008): 303–13. http://dx.doi.org/10.1016/j.fishres.2008.01.014.

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29

Robson, B. J., and B. D. Mitchell. "Metastability in a river subject to multiple disturbances may constrain restoration options." Marine and Freshwater Research 61, no. 7 (2010): 778. http://dx.doi.org/10.1071/mf09073.

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Metastability may arise in rivers subject to multiple disturbance processes because external constraints to ecosystem change sustain the metastable state; this has important implications for management, especially river restoration. The Glenelg River and its southern Australian landscape have been extensively studied by different researchers across many projects, and several restoration actions implemented across different reaches and spatial scales. Research involving diverse researchers and projects over extended periods shows strengths such as flexibility in pursuing emerging research questions, increased regional capacity by facilitating research training, and the generation of broader perspectives on river management. We conclude that metastability is a likely state for rivers with multiple interacting disturbances in regions with Mediterranean-type climates. In such rivers, disrupted relationships between the physical environment and ecological processes are likely, such that habitat restoration might have limited effectiveness. Restoration practices that constitute a disturbance might also risk disrupting metastability, or their impact may be limited because metastability confers resistance to further disturbance. Restoration may be more effectively targeted at less-disturbed reaches where ecosystems have a greater capacity to respond. Similarly, restoration in disturbed reaches might be more effectively directed at supporting metastability in the face of landscape change, than attempting to restore antecedent conditions.

30

Honan, JA, and BD Mitchell. "Reproduction of Euastacus bispinosus Clark (Decapoda:Parastacidae), and trends in the reproductive characteristics of freshwater crayfish." Marine and Freshwater Research 46, no. 2 (1995): 485. http://dx.doi.org/10.1071/mf9950485.

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The reproductive biology of Euastacus bispinosus populations was studied in a river and a creek of the Glenelg River system in south-western Victoria, and a small coastal creek in south-eastern South Australia. Females produced eggs in the first breeding season after maturation of their gonopores. At the Victorian sites, E. bispinosus spawned in early May, carrying eggs for about seven months before hatching and juvenile release in October-December. At least 95% of mature females at each Victorian site carried eggs during the breeding season. Mature females had relatively broader abdomens than did males and carried between 63 and 812 eggs. The number of eggs carried was linearly related to both occipital carapace length and abdomen width. The South Australian population differed from the Victorian populations in having a smaller mean size at sexual maturity for females (occipital carapace length 58 mm compared with 85-86 mm in Victoria), a higher proportion (17%) of gonopore abnormalities (< 1% in Victoria), and relatively wider abdomens (which continued to broaden after maturity). Euastacus bispinosus is a winter brooder and has a long generation time and low potential reproductive rate, characteristics it shares with Astacopsis and Parastacoides species, and members of the Astacidae. Other crayfish species (e.g. Cherax species and members of the Cambaridae) are summer brooders and tend to have a high potential reproductive rate and short generation time.

31

Unmack, P. J., M. J. Young, B. Gruber, D. White, A. Kilian, X. Zhang, and A. Georges. "Phylogeography and species delimitation of Cherax destructor (Decapoda: Parastacidae) using genome-wide SNPs." Marine and Freshwater Research 70, no. 6 (2019): 857. http://dx.doi.org/10.1071/mf18347.

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Cherax is a genus of 58 species of decapod crustaceans that are widespread across Australia and New Guinea. We use single-nucleotide polymorphisms (SNPs) to examine phylogeographic patterns in the most widespread species of Cherax, namely, C. destructor, and test the distinctiveness of one undescribed species, two C. destructor subspecies, previously proposed evolutionarily significant units, and management units. Both the phylogenetic analyses and the analysis of fixed allelic differences between populations support the current species-level taxonomy of C. setosus, C. depressus, C. dispar and C. destructor, the distinctiveness of C. destructor albidus and C. d. destructor and the existence of one undescribed species. The two populations of C. d. albidus from the Glenelg and Wimmera rivers were significantly distinct, with eight diagnostic differences (<1% fixed differences, null expectation is four fixed differences), but this low level of divergence is interpreted as within the range that might be expected of management units, that is, among allopatric populations of a single species or subspecies. A southern clade of C. d. destructor comprising the Murray River and its tributaries upstream from its confluence with the Darling River is genetically distinct from a northern clade comprising populations from the Lake Eyre Basin, the northern half of the Murray–Darling Basin (Darling River catchment) and the Lower Murray River below the Darling confluence.

32

Fyffe, Leslie R., and William W. Gardiner. "Investigation of Sheriff Stuart’s black granite quarries in Charlotte County, southwestern New Brunswick: implications for the source of the titanic headstones in Halifax, Nova Scotia." Atlantic Geology 56 (September 13, 2020): 189–206. http://dx.doi.org/10.4138/atlgeol.2020.008.

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Robert Albert Stuart, the High Sheriff of Charlotte County, deserves credit for establishing the black granite monument industry in New Brunswick. In the late 19th to early 20th centuries, he opened three quarries in mafic plutonic rocks in the vicinity of the Chickahominy Mountain, north of St. Andrews: the Bocabec black granite quarry (1893), the Steen Lake black granite quarry (1895), and the Glenelg porphyry quarry (1906). Much of the information in brief articles in local newspapers lacks sufficient detail to gain a full understanding of the historical development of these quarries. To obtain a clearer timeline for production of stone from the quarries, the rock type in each was examined and compared to black granite monuments in nearby cemeteries known to be sourced from these specific quarries. Previous investigations did not entirely rule out the possibility that the Stuart quarries may have been a source for the headstones placed in the Fairview Lawn Cemetery in Halifax, Nova Scotia, to mark the graves of some of those who were lost when the Titanic sank in 1912. Our detailed analysis of rock textures and production histories leads us to conclude that none of the Stuart quarries could have been a source for the Titanic headstones and supports the previous assessment that they came from Charles Hanson quarry.

33

Kemp, A. I. S. "Petrology of high-Mg, low-Ti igneous rocks of the Glenelg River Complex (SE Australia) and the nature of their interaction with crustal melts☆." Lithos 78, no. 1-2 (October 2004): 119–56. http://dx.doi.org/10.1016/j.lithos.2004.04.044.

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34

Krabbendam, M., J. G. Ramsay, A. G. Leslie, P. W. G. Tanner, D. Dietrich, and K. M. Goodenough. "Caledonian and Knoydartian overprinting of a Grenvillian inlier and the enclosing Morar Group rocks: structural evolution of the Precambrian Proto-Moine Nappe, Glenelg, NW Scotland." Scottish Journal of Geology 54, no. 1 (November 21, 2017): 13–35. http://dx.doi.org/10.1144/sjg2017-006.

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35

Miller, Adam D., Anthony Van Rooyen, Oisín F. Sweeney, Nick S. Whiterod, and Andrew R. Weeks. "The development of 10 novel polymorphic microsatellite markers through next generation sequencing and a preliminary population genetic analysis for the endangered Glenelg spiny crayfish, Euastacus bispinosus." Molecular Biology Reports 40, no. 7 (May 4, 2013): 4415–19. http://dx.doi.org/10.1007/s11033-013-2531-5.

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36

Weston, Janice F., R. Andrew MacRae, Piero Ascoli, M. Kevin E. Cooper, Robert A. Fensome, David Shaw, and Graham L. Williams. "A revised biostratigraphic and well-log sequence-stratigraphic framework for the Scotian Margin, offshore eastern Canada 1This article is one of a series of papers published in this CJES Special Issue on the theme of Mesozoic–Cenozoic geology of the Scotian Basin. 2Earth Sciences Sector Contribution 20120137." Canadian Journal of Earth Sciences 49, no. 12 (December 2012): 1417–62. http://dx.doi.org/10.1139/e2012-070.

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In this study, we build on a foundation of previous biostratigraphic studies for the Scotian Basin, offshore eastern Canada, by conducting new quantitative multidisciplinary biostratigraphic studies of the Mesozoic sections in eight wells: Bonnet P-23, Chebucto K-90, Cohasset L-97, Glenelg J-48, Glooscap C-63, Mohican I-100, South Desbarres O-76, and South Griffin J-13. These wells were chosen to provide good spatial coverage, stratigraphic penetration, and correlation with the seismic grid. We have also evaluated pre-existing biostratigraphic data and undertaken the well-log sequence-stratigraphic interpretation of Upper Triassic to Cenozoic sediments in 16 additional wells using a consistent multidisciplinary event scheme derived from the new wells. Key to the dating of some horizons has been integration of the palynology and micropaleontology (disciplines mostly used previously on the Scotian Margin) with new nannofossil data. Simultaneously we have closely integrated the biostratigraphic results with lithofacies, well-log, and seismic interpretations. Using this integrated approach, we have identified nine regionally mappable sequence-stratigraphic events (unconformities and maximum flooding surfaces, or MFSs): the Intra-Oligocene Unconformity; the Ypresian Unconformity; the Turonian/Cenomanian Unconformity; the Late Albian Unconformity; the Aptian/Barremian Unconformity; the Intra-Hauterivian MFS; the Near-Base Cretaceous Unconformity; the Tithonian MFS; and the Top-Callovian MFS. Additional events of local extent were also recognized in some wells. Our study has led to significant revision of some previous lithostratigraphic picks. The Early Jurassic on the Scotian Margin remains poorly resolved and may be represented by an unconformity on much of the basin periphery.

37

Fukuda, Hiroshi, and Winston F. Ponder. "A revision of the Australian taxa previously attributed to Assiminea buccinoides (Quoy & Gaimard) and Assiminea tasmanica Tenison-Woods (Mollusca:Gastropoda:Caenogastropoda:Assimineidae)." Invertebrate Systematics 19, no. 4 (2005): 325. http://dx.doi.org/10.1071/is04009.

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A new genus, Cryptassiminea, is introduced for the taxon previously known as Assiminea buccinoides (Quoy & Gaimard). These small gastropods are abundant in mangrove and salt marsh habitats in south-eastern and subtropical eastern Australia. Seven species (five new) are recognised using morphological characters in the complex previously treated as a single species. Five taxa have rather narrow ranges while the other two are widespread and often sympatric. Two groups of species are recognised. One contains Cryptassiminea buccinoides, widespread in south-east and east Australia, and two closely related allopatric taxa from South Australia and south-eastern Tasmania (C. adelaidensis, sp. nov. and C. kershawi, sp. nov.). A second group of species is typified by Cryptassiminea tasmanica (Tenison-Woods), also widespread in east and south-east Australia and often sympatric with C. buccinoides. Allied to C. tasmanica, are two closely related taxa from western Victoria: C. glenelgensis, sp. nov. from the Glenelg River estuary and C. surryensis, sp. nov. from the Surry River estuary and Western Port, in the vicinity of Geelong. A distinctive species, Cryptassiminea insolata, sp. nov. from the east coast of Queensland, also has similarities with C. tasmanica. A cladistic analysis using morphological characters of the Cryptassiminea taxa and three other genera of Assimininae, with an omphalotropidine as the outgroup, resulted in a single tree. The new genus has rather poor support, possibly because many of its characters appear to be plesiomorphic within Assimineinae. Cryptassiminea is defined by a unique combination of characters but lacks any obvious synapomorphy. Two clades within Cryptassiminea are well supported, each containing the species-groups referred to above.

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LESTER, ALAN. "SETTLERS, THE STATE AND COLONIAL POWER: THE COLONIZATION OF QUEEN ADELAIDE PROVINCE, 1834–37." Journal of African History 39, no. 2 (July 1998): 221–46. http://dx.doi.org/10.1017/s0021853797007184.

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Queen Adelaide Province consisted of some 7,000 square miles of Rarabe Xhosa territory annexed by the British Cape colonial government in May 1835 during the Sixth Frontier War. The province was held only until the end of 1836 when it was abandoned under pressure from the imperial government, but it represented the first British attempt to extend direct control over a large body of formerly independent Africans. No such ambitious scheme had ever been attempted before in the Cape, and no such scheme was to be attempted elsewhere in Africa until the late nineteenth century.Given its short-lived nature, Queen Adelaide Province has not been extensively analysed in any of the prominent histories of the eastern Cape. However, while the treatment is brief, its significance has been widely recognized. This early, temporary colonization of Xhosa territory has served as a lens through which to view colonial extension in the eastern Cape as a whole. In the late-nineteenth and early twentieth-century settler histories of George Cory and George McCall Theal, the annexation of Queen Adelaide Province represents a temporary advance within a much broader colonial progress. One episode in the epic attempt to extend colonial civilization across ‘Kaffraria’, expansion within the province was unfortunately thwarted by misguided Cape and metropolitan philanthropy. In W. M. Macmillan's liberal critique of the late 1920s and early 1930s, the disputes over the province between the land-hungry settlers, the strategically-minded Governor D'Urban and the humanitarian Secretary of State for the Colonies, Lord Glenelg, are again viewed as part of a much broader struggle. But rather than Cory's struggle between civilization and savagery, this is seen as a contest between malicious and benign conceptions of colonialism. The province represents an early collision between, on the one hand, evangelical and humanitarian versions of cultural colonization that guaranteed Xhosa access to their land (a kind of trusteeship that Macmillan advocated for his own times) and, on the other hand, the practice of colonization founded upon settler-led conquest and dispossession.

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Officer, S. J., R. D. Armstrong, and R. M. Norton. "Plant availability of phosphorus from fluid fertiliser is maintained under soil moisture deficit in non-calcareous soils of south-eastern Australia." Soil Research 47, no. 1 (2009): 103. http://dx.doi.org/10.1071/sr08090.

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Low soil moisture and phosphorus (P) deficiencies restrict grain production in south-eastern Australia. The effect of the soil moisture regime on the plant availability of P from fluid mono-ammonium phosphate (MAP) fertiliser was examined during vegetative growth of wheat and canola in P-responsive soils from the Wimmera, Mallee, and high rainfall zone (Glenelg) regions of Victoria. Three plant growth experiments were performed. In Experiment 1, wheat growth and P uptake increased synergistically as soil moisture increased above permanent wilting point (PWP) and as P rate increased. In Experiment 2, the uptake of P from MAP fertiliser of wheat growing under a soil moisture deficit was examined using radioactive (32P) labelling. A factorial design compared uptake from intact soil cores of 3 soil types (Vertosol, Sodosol, Chromosol), 2 depths of fertiliser placement (40 and 80 mm), and either 0 or 25 kg P/ha. Results showed distinct plant responses to both the presence and depth of MAP fertiliser. Banding MAP close to the seed was most efficient in terms of recovery of the fertiliser P, regardless of the soil moisture conditions. Soil moisture regime affected the plant uptake of soil P, rather than fertiliser P, with more soil P taken up by the plants when soil moisture increased. The plant availability of the residual MAP fertiliser in the soil was subsequently examined in Experiment 3. The availability of the residual MAP to canola seedlings was equivalent to 8 kg P/ha of freshly applied MAP. Following both crops (9 months), Colwell P values indicated no further residual MAP availability in soil that had been under the wet regime, and only a small residual value in soil from the dry regime. Banded application of fluid MAP close to the seed and into soil that is above PWP is recommended, even when a relatively dry season is expected, although the residual value to following crops may be limited.

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Glenberg, Arthur M., David A. Robertson, Michael P. Kaschak, and Alan J. Malter. "Embodied meaning and negative priming." Behavioral and Brain Sciences 26, no. 5 (October 2003): 644–47. http://dx.doi.org/10.1017/s0140525x03240140.

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Standard models of cognition are built from abstract, amodal, arbitrary symbols, and the meanings of those symbols are given solely by their interrelations. The target article (Glenberg 1997t) argues that these models must be inadequate because meaning cannot arise from relations among abstract symbols. For cognitive representations to be meaningful they must, at the least, be grounded; but abstract symbols are difficult, if not impossible, to ground. As an alternative, the target article developed a framework in which representations are grounded in perception and action, and hence are embodied. Recent work (Glenberg & Robertson 1999; 2000; Glenberg & Kaschak 2002; Kaschak & Glenberg 2000) extends this framework to language.

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Jacobs, Arthur M., and Johannes C. Ziegler. "Has Glenberg forgotten his nurse?" Behavioral and Brain Sciences 20, no. 1 (March 1997): 26–27. http://dx.doi.org/10.1017/s0140525x97310012.

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Glenberg's conception of “meaning from and for action” is too narrow. For example, it provides no satisfactory account of the “logic of Elfland,” a metaphor used by Chesterton to refer to meaning acquired by being told something.All that we call spirit and art and ecstasy only means that for one awful instant we remember that we forget.G. K. Chesterton (in Gardner 1994, p. 101)

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MONNÉ, MIGUEL A., FRANCISCO E. DE L. NASCIMENTO, MARCELA L. MONNÉ, and ANTONIO SANTOS-SILVA. "New records, new genera, and new species in Acanthocinini (Lamiinae) from the Neotropical region, and new synonym in Cerambycinae (Coleoptera, Cerambycidae)." Zootaxa 4624, no. 4 (July 2, 2019): 491–506. http://dx.doi.org/10.11646/zootaxa.4624.4.3.

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Notes and new country records are provided for Leptostylus retrorsus Bates, 1885, and Lagocheirus araneiformis flavolineatus Aurivillius, 1921. The male of Trichalcidion penicillum Monné & Delfino, 1981 is described for the first time, and a new country record is provided. One new genus and four new species are described: Vitacinis luziae from Colombia (new genus); Nealcidion antonkozlovi from Colombia; Onalcidion antonkozlovi from Colombia; and Leptocometes antonkozlovi from Colombia. Hemilocallia grishami Ramírez Hernández et al., 2019 is synonymized with Glenea (Glenea) fasciata (Fabricius, 1781) [Hemilocallia = Glenea (Glenea); H. grishami = G. (G.) fasciata].

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MacDorman, Carl F. "Memory must also mesh affect." Behavioral and Brain Sciences 20, no. 1 (March 1997): 29–30. http://dx.doi.org/10.1017/s0140525x97340011.

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To model potential interactions, memory must not only mesh prior patterns of action, as Glenberg proposes, but also their internal consequences. This is necessary both to discriminate sensorimotor information by its relevance and to explain how go als about the world develop. In the absence of internal feedback, Glenberg is forced to reintroduce a grounding problem into his otherwise sound model by presupposing interactive goals.

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Humphreys, D. G., T. F. Townley-Smith, O. Lukow, B. McCallum, D. Gaudet, J. Gilbert, T. Fetch, J. Menzies, D. Brown, and E. Czarnecki. "Burnside extra strong hard red spring wheat." Canadian Journal of Plant Science 90, no. 1 (January 1, 2010): 79–84. http://dx.doi.org/10.4141/cjps09100.

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Burnside is a hard, red, spring wheat (Triticum aestivum L.) that meets the end-use quality specifications of the Canada Western Extra Strong wheat class. Burnside was evaluated in the Canada Western Extra Strong Wheat Cooperative Test in 2000, 2001, and 2002. In comparison with CWES cultivars Glenlea, Bluesky, AC Corinne, and CDC Walrus, Burnside had higher grain yields than Bluesky and AC Corinne, was similar to Glenlea and lower yielding than CDC Walrus. Burnside had maturity similar to Bluesky and was earlier maturing than Glenlea, AC Corinne, and CDC Walrus. Burnside is resistant to moderately resistant to prevalent races of leaf and stem rust and resistant to loose smut. End-use quality tests showed that Burnside had significantly higher grain protein content than the check cultivars.Key words: Triticum aestivum L., Canada Western Extra Strong, hard red extra strong spring wheat, cultivar description, yield, disease resistance

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LIN, MEIYING, GÉRARD TAVAKILIAN, OLIVIER MONTREUIL, and XINGKE YANG. "Eight species of the genus Glenea Newman, 1842 from the Oriental Region, with description of three new species (Coleoptera: Cerambycidae: Lamiinae: Saperdini)." Zootaxa 2155, no. 1 (July 13, 2009): 1–22. http://dx.doi.org/10.11646/zootaxa.2155.1.1.

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Eight species of Glenea Newman, 1842 from the Oriental Region are studied, including description of three new species: G. paradiana Lin et Montreuil sp. nov. from Vietnam & Laos, G. nigrorubricollis Lin et Yang sp. nov. from Guangdong, China and G. subrubricollis Lin et Tavakilian sp. nov. from Vietnam. Glenea theresae Pic, 1943 is regarded as a junior synonym of G. diana Thomson, 1865, and G. (Mesoglenea) invitticollis Breuning, 1956 as a junior synonym of G. flavorubra Gressitt, 1940. Glenea rufipes Gressitt, 1939 is reinstated from synonym of G. subsimilis Gahan, 1897. Habitus and terminalia are presented as photographs.

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Humphreys, D. G., T. F. Townley-Smith, R. I. H. McKenzie, and E. Czarnecki. "AC Corinne hard red spring wheat." Canadian Journal of Plant Science 81, no. 4 (October 1, 2001): 741–43. http://dx.doi.org/10.4141/p00-167.

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AC Corinne is a hard red spring wheat belonging to the Canada Western Extra Strong (CWES) class. It has superior preharvest sprouting resistance and improved leaf rust resistance compared to Glenlea and Wildcat, and is higher yielding than Wildcat. AC Corinne has extra strong wheat quality similar to Glenlea combined with higher grain protein content. It is adapted to the wheat growing areas of the prairie provinces. Key words: Triticum aestivum L., Canada Western Extra Strong, hard red spring wheat, cultivar description, yield, disease resistance

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Jedel, P. E. "Inheritance of vernalization response in three populations of spring wheat." Canadian Journal of Plant Science 74, no. 4 (October 1, 1994): 753–57. http://dx.doi.org/10.4141/cjps94-134.

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Vernalization responses are known to differ among spring wheat (Triticum aestivum L.) genotypes. Three crosses were made to determine the inheritance of vernalization response in the spring wheat cultivars Cajeme 71, Yecora 70, Glenlea, Pitic 62 and Neepawa. Segregation analyses of days to anthesis were made of the F2 generation in a growth room (25/15 °C, 16/8 h). Segregation analysis of the F3 generation was made in a summer greenhouse. Reciprocal crosses between Neepawa and Pitic 62 indicated an early/late/transgressively late ratio of 12:3:1 in the F2 generation. The F3 generation results fitted an early/late/transgressively late/segregating ratio of 4:1:1:10. Based on the segregation of transgressively late types from both crosses, it was concluded that the genes for spring habit in Pitic 62 and Neepawa were different and not maternally inherited. The Glenlea/Pitic 62 cross produced one transgressively late segregant in an F2 population of 97 plants. The data fitted an early/late/transgressively late ratio of 60:3:1, indicating that Glenlea may differ from Pitic at three Vrn loci. Therefore, either Glenlea or Pitic 62 may carry two dominant Vrn alleles. The reciprocal crosses between Yecora 70 and Cajeme 71 did not segregate transgressively late types in the F2 generation. Therefore, those cultivars had a Vrn allele in common. Selection for vernalization response might be useful when introducing exotic germplasm into spring wheat breeding programs and in manipulating maturity responses. Key words: Vernalization, spring wheat, Vrn genes

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Rodríguez-García, María F., Reyna I. Rojas-Martínez, Julio Huerta-Espino, Héctor E. Villaseñor-Mir, Emma Zavaleta-Mejía, José S. Sandoval-Islas, and José F. Crossa-Hiriart. "GENÉTICA DE LA RESISTENCIA A ROYA AMARILLA CAUSADA POR Puccinia striiformis f. sp. tritici W. EN TRES GENOTIPOS DE TRIGO (Triticum aestivum L.)." Revista Fitotecnia Mexicana 42, no. 1 (February 15, 2019): 31–38. http://dx.doi.org/10.35196/rfm.2019.1.31-38.

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La roya amarilla del trigo causada por Puccinia striiformis f. sp. tritici se ha convertido en una enfermedad de importancia a nivel mundial en los últimos años. La resistencia genética en variedades es la estrategia más efectiva para el control de esta enfermedad. En la actualidad existen genotipos de trigo que han mostrado resistencia en diferentes años y ambientes de producción. El objetivo del presente estudio fue determinar el tipo de resistencia y estimar el número de genes que condicionan la resistencia a roya amarilla en los genotipos Glenlea, Romero 73 y Bonza 63. Se utilizó como progenitor susceptible a Avocet-YrA, se generaron tres poblaciones, las cuales se avanzaron hasta obtener familias F5. Las poblaciones se evaluaron en un ensayo con un diseño experimental de bloques completos al azar, bajo epidemias artificiales del hongo causante de la roya amarilla, en la estación experimental del INIFAP-CEVAMEX en Chapingo, México, durante el ciclo primavera-verano (P-V) 2015. La formación de rocío al 100 % y temperaturas entre 10 y 20 ºC fueron favorables para el desarrollo de la enfermedad, lo que permitió determinar que la resistencia de Bonza 63, Glenlea y Romero 73 se debe al efecto de genes menores de tipo cuantitativo. El comportamiento de las familias y el análisis de X2 indicó la presencia de tres genes que confieren resistencia de planta adulta (RPA) a roya amarilla en los genotipos Bonza 63 y Romero 73. Se determinó que la variedad Glenlea posee de cuatro a cinco genes de RPA. Bonza 63, Glenlea y Romero 73 poseen altos niveles de resistencia en planta adulta a las diversas razas presentes en las principales regiones trigueras de México y son adecuados para usarse como progenitores en los programas de mejoramiento para lograr una resistencia durable a roya amarilla.

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CONNER, R. L., and J. G. N. DAVIDSON. "RESISTANCE IN WHEAT TO BLACK POINT CAUSED BY Alternaria alternata AND Cochliobolus sativus." Canadian Journal of Plant Science 68, no. 2 (April 1, 1988): 351–59. http://dx.doi.org/10.4141/cjps88-046.

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A 2-yr field study conducted at six locations on the Canadian prairies identified seven wheat (Triticum aestivum L. em Thell.) cultivars that consistently had low incidence of black point. These resistant wheats included the hard red spring wheat cultivars Sinton, Park, Thatcher, Benito and Era, the utility wheat Glenlea, and the soft white spring wheat line SWS15 (ICARDA 15). In separate tests, the inoculation of resistant wheat cultivars with Alternaria alternata (Fr.) Keissler or Cochliobolus sativus (Ito and Kurib.) Drechs. ex Dastur under controlled environmental conditions revealed significant differences in black point incidence. All cultivars were more resistant to A. alternata than the susceptible cultivar Fielder. Glenlea and Era were more resistant to A. alternata than all the other cultivars. Only the cultivars Thatcher, Benito, and Sinton were more resistant to C. sativus than Fielder. A test comparing black point incidence caused by the two fungi found that certain cultivars differed significantly in disease incidence caused by A. alternata and C. sativus. Cochliobolus sativus produced less disease in Fielder and Sinton than A. alternata, but the reverse was true for Glenlea. These results indicate that resistance to A. alternata and C. sativus is under different genetic control in certain cultivars.Key words: Wheat (spring), black point, Alternaria alternata, Cochliobolus sativus

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Humphreys, D. G., B. D. McCallum, T. G. Fetch, J. A. Gilbert, O. M. Lukow, J. G. Menzies, P. D. Brown, and S. L. Fox. "Glencross hard red extra strong spring wheat." Canadian Journal of Plant Science 100, no. 1 (February 1, 2020): 121–28. http://dx.doi.org/10.1139/cjps-2019-0191.

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Glencross is a hard red spring wheat (Triticum aestivum L.) adapted to the wheat-growing regions of the Canadian Prairies, particularly where orange blossom wheat midge is a production constraint. Glencross was evaluated in the High Yielding Red Wheat Cooperative Test in 2004, 2005, and 2006. Glencross had grain yield similar to the Canada Western Extra Strong (CWES) checks, Glenlea and CDC Rama, as well as the Canada Western Red Spring check, Superb; however, Glencross was significantly (P < 0.05) earlier maturing than all checks by 3 (Superb) to 4 (Glenlea and CDC Rama) days. Glencross had plant height and lodging scores similar to the CWES checks, Glenlea and CDC Rama, but was significantly taller and had significantly higher lodging scores compared with the CWRS check, Superb. Glencross was moderately resistant to moderately susceptible to leaf rust but was highly resistant to stem rust and loose smut. Glencross showed an intermediate reaction to common bunt and was similar to the susceptible checks for Fusarium head blight. Glencross is the first CWES cultivar with resistance to the orange blossom wheat midge (Setodiplosis mosellana Géhin). Glencross demonstrated end-use quality suitable for all grades of the Canada Western Extra Strong wheat class.