The ghost bat in the Pilbara: 100 years on.

2000 ◽  
Vol 22 (2) ◽  
pp. 93 ◽  
Author(s):  
KN Armstrong ◽  
SD Anstee

This paper summarises the roost habitat and distribution of the ghost bat, Macroderma gigas (Dobson, 1880), in the Pilbara region of Western Australia, with particular emphasis on natural habitats. The preferred habitat of M. gigas in the Hamersley Ranges appears to be caves beneath bluffs of low rounded hills composed of Marra Mamba geology. Habitats were also found in the larger hills of Brockman Iron Formation in the Hamersley Range, and other formations beneath bluffs composed of Gorge Creek Group geology to the north east. Granite rockpiles are also used in the eastern Pilbara. A summary of Pilbara records from numerous sources is presented, including anecdotal accounts and other new records. This includes a newly discovered maternity site from the Hamersley Ranges, only the third reported from natural cave formations in the region. Threats to M. gigas in the region are highlighted and include disturbances associated with mining and entanglement in barbed wire fences.

Author(s):  
Peter R. Dawes ◽  
Bjørn Thomassen ◽  
T.I. Hauge Andersson

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Dawes, P. R., Thomassen, B., & Andersson, T. H. (2000). A new volcanic province: evidence from glacial erratics in western North Greenland. Geology of Greenland Survey Bulletin, 186, 35-41. https://doi.org/10.34194/ggub.v186.5213 _______________ Mapping and regional geological studies in northern Greenland were carried out during the project Kane Basin 1999 (see Dawes et al. 2000, this volume). During ore geological studies in Washington Land by one of us (B.T.), finds of erratics of banded iron formation (BIF) directed special attention to the till, glaciofluvial and fluvial sediments. This led to the discovery that in certain parts of Daugaard-Jensen Land and Washington Land volcanic rocks form a common component of the surficial deposits, with particularly colourful, red porphyries catching the eye. The presence of BIF is interesting but not altogether unexpected since BIF erratics have been reported from southern Hall Land just to the north-east (Kelly & Bennike 1992) and such rocks crop out in the Precambrian shield of North-West Greenland to the south (Fig. 1; Dawes 1991). On the other hand, the presence of volcanic erratics was unexpected and stimulated the work reported on here.


1964 ◽  
Vol 44 (1) ◽  
pp. 1-8

Early in 1963 much of the land occupied by the Roman building at Fishbourne was purchased by Mr. I. D. Margary, M.A., F.S.A., and was given to the Sussex Archaeological Trust. The Fishbourne Committee of the trust was set up to administer the future of the site. The third season's excavation, carried out at the desire of this committee, was again organized by the Chichester Civic Society.1 About fifty volunteers a day were employed from 24th July to 3rd September. Excavation concentrated upon three main areas; the orchard south of the east wing excavated in 1962, the west end of the north wing, and the west wing. In addition, trial trenches were dug at the north-east and north-west extremities of the building and in the area to the north of the north wing. The work of supervision was carried out by Miss F. Pierce, M.A., Mr. B. Morley, Mr. A. B. Norton, B.A., and Mr. J. P. Wild, B.A. Photography was organized by Mr. D. B. Baker and Mrs. F. A. Cunliffe took charge of the pottery and finds.


1991 ◽  
Vol 71 ◽  
pp. 191-215 ◽  
Author(s):  
Svend Helms

Qaṣr Burqu⃓ is one of the most remote of the Jordanian so-called ‘desert castles’ (quṣūr) of the early Islamic period: it lies some 200km east of⃓Ammān (figs. 1–4). However, it is neither a castle, nor is it in the desert, rather it represents a variety of building types and lies in the dry steppe (areas receiving less than 100mm of rainfall per annum) of the bādiyat al-šām (literally, the steppe lands of Damascus). Furthermore, most of the architectural elements are not necessarily attributable to the early Islamic period, namely the Umayyad Caliphate of the seventh and eighth centuries, despite a ‘building’ inscription (E4: see below, pp. 206–7) of Walīd b. ‘Abd’l-Malik (Caliph AD 705–15), dated AD 700 (H. 81). Rather, the various architectural entities at the site, and their use, span the time from about the third-fourth (probably a little later) to the eighth centuries AD. This time range and the Qaṣr's remote location are significant in relation to the political and economic history of the Near East, particularly in regard of nomad-state relations across the verdant-steppic interface. The time range of the various constructions includes the period following the dissolution of the limes arabicus which had been extensively refurbished and augmented under Diocletian and later under Justinian in the third and sixth centuries AD. Many of the more remote erstwhile fortlets, forts and legionary fortresses were colonized by villagers and nomads, as well as monks and pious hermits. Between the fourth and sixth centuries (particularly in the sixth century under the Ghassānids), purpose-built monasteries and ‘residences’ for hermits were established throughout greater Syria, some of them far out in the steppe. The military station at Nemāras about 80km to the north-east of Qaṣr Burqu⃓, for example, may have become one of several centres, functioning as a παƍεμβολή νομάδον of the Lakhmids in the region, under the leadership of Imru'l-Qays who was called ‘king of the Arabs’ and who was buried there in AD 328. Places like Qaṣr Burqu⃓ and Deir al-Kinn, on the other hand, may have been founded or re-established as monasteries.


1982 ◽  
Vol 14 (2) ◽  
pp. 139-152 ◽  
Author(s):  
H. Hertel ◽  
C.-F. Zhao

AbstractTwenty-five mainly crustose and saxicolous lichens are reported from the subalpine and alpine belts of Mt Changbai (n.-e. China, near the Korean border). All are new records to the lichen flora of the north-eastern provinces of China, 12 of them to the flora of all China, and four to the flora of all Asia. There is some floristic similarity to some other areas with cool humid climates in the Northern Hemisphere, e.g. Iceland.


Phytotaxa ◽  
2013 ◽  
Vol 101 (1) ◽  
pp. 1 ◽  
Author(s):  
ZOË A. GOODWIN ◽  
GERMAN N. LOPEZ ◽  
NEIL STUART ◽  
SAMUEL G.M. BRIDGEWATER ◽  
ELSPETH M. HASTON ◽  
...  

 Lowland savannas, covering an area of 2,342 km2, form the third largest ecosystem in Belize yet are unevenly and therefore poorly represented in the country’s protected area system. Based on more than 5,700 herbarium collections, a checklist of 957 species of vascular plants is presented for this ecosystem representing ca. 28% of the Belizean flora, of which 54 species are new records for the country. Of the 41 species of plants known to be endemic to Belize, 18 have been recorded within the lowland savanna, and nine species are listed in The World Conservation Union (IUCN) 2010 Red List of Threatened Species. Of the total savanna ecosystem flora, 339 species are characteristic of the open savanna, whilst 309 and 114 species are more frequent in forest and wetland areas respectively. Most species (505, 53% of the lowland savanna flora) are herbaceous. Although the lowland savanna has been relatively well collected, there are geographical biases in botanical sampling which have focused historically on the savannas in the centre and the north of the country. A brief review of the collecting history of the lowland savanna is provided, and recommendations are given on how future collecting efforts may best be focused. The lowland savanna is shown to be a significant regional centre of plant diversity.


Zootaxa ◽  
2010 ◽  
Vol 2389 (1) ◽  
pp. 57 ◽  
Author(s):  
ELENA K. KUPRIYANOVA ◽  
EIJIROH NISHI ◽  
MASARU KAWATO ◽  
YOSHIHIRO FUJIWARA

Serpulidae are sessile suspension-feeding annelids commonly found in the periphery of hydrothermal vents, but up to now only two species, Laminatubus alvini and Protis hydrothermica had been described from such communities. This paper reports two additional serpulid species, collected in 2005 from the North Fiji hydrothermal vent area, identified as Hyalopomatus mironovi and Protis sp. The former has originally been described from the Kurile-Kamchatka Trench and the later recorded from the North-East Pacific. The latter species is similar to Protis hydrothermica, but lacks special finand-blade collar chaetae typical of this genus. Illustrated re-descriptions of the two species have been supplemented by molecular sequences (18S ribosomal RNA). Molecular phylogenetic analyses show that Hyalopomatus mironovi and Protis sp. are sister species of Laminatubus alvini and Protis hydrothermica, respectively.


2016 ◽  
Vol 30 (2) ◽  
pp. 155-167 ◽  
Author(s):  
Derek Watson ◽  
Lynne Hall ◽  
Sarah Tazzyman

This paper reports in part on a major study, carried out in 2013, in which data were collected from university senior executives and academics in the five university business schools in the North East of England: it focuses on the quantitative findings produced. Whilst prima facie evidence would suggest that universities are strategically embedding and integrating third stream strategies alongside first and second stream activities, a critical analysis of the research data revealed that this was clearly not the case. Empirical evidence from the research indicates that there are strategic failings in universities. This research contributes to the existing literature which highlights the academic pressures in embedding the third stream in higher education institutions.


Author(s):  
Frederic Olivier ◽  
Paulo Lana ◽  
Veronica Oliveira ◽  
Tim Worsfold

We describe Dysponetus joeli sp. nov. from shallow maerl habitats in the north-east Atlantic (English Channel and Bay of Biscay). Dysponetus joeli differs from congeneric species by a unique combination of characters, including a large syllid-like pharynx, 2–4 simple serrated neurochaetae (closely similar to notochaetae, but much smaller and more delicate), D-shaped chaetal spines and ventral cirri on the third segment. A phylogenetic parsimony analysis based on morphological traits suggests that Dysponetus is not monophyletic unless it includes the closely related genera Vigtorniella and Pseudodysponetus, which are well delineated inside the dysponetid clade. Chaetal spines seem to be secondarily derived from paleae and to have originated in infaunal dysponetid forms. They should not be considered as plesiomorphic, but as evidence to support the clade made up by Dysponetus–Vigtorniella and Pseudodysponetus as delineated by a phylogenetic analysis.


Author(s):  
Iván Enrique Caycedo

Systematic and ecological remarks are presented on 14 species of shallow water holothurians of the northern coast of Colombia. The material was collected from Islas del Rosario off the coast southwest of Cartagena (10° 08' 39" Lat. N 75° 43, 21" Long. W) and from Tayrona National Park to the north east of Santa Marta (11° 20, Lat. N and 74 05, Long. W). Ten species are new records to Colombia, one of them appeared to be undescribed as yet (Holothuria thomaú sp. nov. Pawson & Caycedo, in preparation). A key to these species is given. The occurrence of some species in abundance in different habitats is discussed in order to elucidate ecological interrelationships and facilitate field identification.


Author(s):  
North East Third Sector Research Group

<p>This inaugural Digest Review is the culmination of the efforts of a group of people working to increase levels of engagement between academia and the Third Sector. Those who have submitted formal contributions have spent time and effort developing thoughtful and honest reflections and for that, we are truly thankful. There are a number of Third Sector professionals and academics who are involved in the North East Third Sector Research Group on an ongoing basis and without that valuable support, the group would not exist. Thank you to everyone involved in the group, as well as this publication. What makes this publication unique is that all of the contributions, editing and design has been done on a voluntary basis.</p><p>Particular thanks must go to Ellen Cole and the team at Northumbria University Library for helping with the technical aspects of copyright notice, attribution and registration.</p>


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