scholarly journals Leptolyngbya sieminskae sp. n. (Cyanobacteria) from Svalbard

2013 ◽  
Vol 34 (2) ◽  
pp. 151-168 ◽  
Author(s):  
Dorota Richter ◽  
Jan Matuła

Abstract This paper describes in detail the phenotypic traits of the newly discovered Leptolyngbya sieminskae sp. n. (Cyanobacteria). The species was found at two islands of the Svalbard archipelago (Spitsbergen and Nordaustlandet) in habitats which differed in humidity, water sources and altitude. The research was conducted at two fjords: on the southern side of Spitsbergen - Hornsund (77ºN, 015ºE) and the north−west side of Nord− austlandet - Murchisonfjord (80ºN, 018ºE). Although Leptolyngbya sieminskae was found in different latitudes no significant morphological differences were found between the specimens from both sites. The only visible difference is in the thickness of filaments and sheaths.

Author(s):  
David Beerling

The Isle of Sheppey lies in the mouth of the Thames tucked up along the northern coastline of Kent, south-eastern England. Known to the Romans as insula orivum, and accessible for centuries only by ferry, the small Isle waited until 1860 for the construction of its first permanent bridge, over the River Swale to the mainland. It contains an uneasy mixture of lowland agricultural farmland, tourism, and commercial shipping activities, all divided by a diagonal east-to-west line of low hills. Elmley Marshes, situated on the southern side of the Isle, attract thousands of ducks, geese, and wading birds in the winter. Further to the east lies the Swale National Nature Reserve, a mosaic of grazing land and salt marshes that is home to short-eared owls and hen harriers. Fine beaches dotted along the northern coastline near to the traditional seaside town of Leysdown-on-Sea draw tourists whose spending boosts the local economy. Discovery of a deep-water channel off the north-west coast saw the construction of a Royal Navy dockyard at Sheerness in 1669. The new dockyard was replaced 290 years later by the commercially successful Port of Sheerness, which benefits from the capacity to accommodate large modern ships regardless of the tides. Geology and the sea have combined to shape the cultural and economic aspects of the Isle from its earliest days. In the early part of the nineteenth century, pyrite—iron sulfide—collected from the beaches and foreshore provided a source of green vitriol dye for the tanning and textiles industries. At around the same time, a small industry flourished excavating cement stones (septaria) for the manufacture of Parker’s (or Roman) cement. But the supply of septarian nodules on the beaches was soon exhausted and, with the emergence of more economic means of producing cement, the industry collapsed. The fleeting septaria industry mirrors the fleeting existence of Sheppey, for the Isle is shrinking fast as wave action erodes metres of its cliffs each year. Ultimately, in no more than a geological instant, the Isle of Sheppey and its inhabitants will be gone.


1913 ◽  
Vol 10 (5) ◽  
pp. 205-215 ◽  
Author(s):  
A. R. Horwood

Although the Rhætic beds are not exposed continuously along the eastern boundary of the Keuper outcrop, they have been proved at many points from the River Trent in the north on the Nottinghamshire border to Glen Parva in the south. South of this point there is so much drift, and borings within the Liassic outcrop have been so isolated or shallow, that there is a gap in our knowledge of the intervening ground between the last point and the Rugby district. The Countesthorpe boring, carried to a depth of over 600 feet, encountered Upper Keuper beneath the Drift, with no intervening Rhætics. Commencing in the north in the Gotham district the two outliers are capped above the Red Marl and Tea-green Marl with Rhætic beds, and Lower Lias Limestone (Ps. planorbe zone) above. At Ash Spinney at the south end of the southern outlier, and at the east end of Crownend Wood, Black Shales with Avicula contorta crop out; and on the west side septaria are seen. On the north-west side of the northern outlier at Cottager's Hill Protocardium phillipianum has been found in a well-section near the lane. Rhætic shales are seen in the shafts driven for gypsum works about Gotham.


Archaeologia ◽  
1779 ◽  
Vol 1 (2) ◽  
pp. 1-7
Author(s):  
Ward
Keyword(s):  
The Hill ◽  

In the year 1740, as I was viewing, with a friend, the church at Burton Dasset in Warwickshire, we happened to observe a painted board placed over the entrance into the chancel, but so covered with dust, that neither we, nor the sexton who attended us, knew what to make of it. But as it seemed to represent something uncommon, we desired we might inspect it somewhat more nearly: And when the sexton had taken it down, and washed it, we perceived it was the picture of a coat of arms, with a Beacon for the crest, (as represented in plate I.) and upon further enquiry we found that, by tradition, there had been formerly a Beacon upon the North-west side of the hill where the church stands, erected by one of the Belknap family, who was then lord of that manor. The board that contains this picture, is nineteen inches and a half in height, and fourteen in breadth. The draught here given of it is reduced to the size of one fourth of the original.


2019 ◽  
Vol 628 ◽  
pp. A69 ◽  
Author(s):  
A. Shulevski ◽  
P. D. Barthel ◽  
R. Morganti ◽  
J. J. Harwood ◽  
M. Brienza ◽  
...  

We have examined the giant radio galaxy 3C 236 using LOFAR at 143 MHz down to an angular resolution of 7″, in combination with observations at higher frequencies. We used the low frequency data to derive spectral index maps with the highest resolution yet at these low frequencies. We confirm a previous detection of an inner hotspot in the north-west lobe and for the first time observe that the south-east lobe hotspot is in fact a triple hotspot, which may point to an intermittent source activity. Also, the spectral index map of 3C 236 shows that the spectral steepening at the inner region of the northern lobe is prominent at low frequencies. The outer regions of both lobes show spectral flattening, in contrast with previous high frequency studies. We derive spectral age estimates for the lobes, as well as particle densities of the IGM at various locations. We propose that the morphological differences between the lobes are driven by variations in the ambient medium density as well as the source activity history.


Author(s):  
Marius Schneider ◽  
Vanessa Ferguson

Burundi is a landlocked country in the Great Lakes region where East and Central Africa meet. It is wedged between Tanzania, the Democratic Republic of the Congo (DRC), and Rwanda. It is a small country of 27,834 square kilometres (km) with a population of 10.8 million in 2017, making it the second most densely populated country in Africa. Since February 2019, Burundi has two capitals: Gitega is the political capital of Burundi while Bujumbura is the economic capital. Bujumbura is also the largest city is and hosts the only international airport, the Bujumbura International Airport. The biggest port of the country is situated on the Lake Tanganyika on the north-west side of Bujumbura. The working week is from Monday to Friday and the currency used is the Burundi Franc (BIF).


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