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Linaria Vulgaris
''Linaria vulgaris'', the common toadflax,Blamey, M. & Grey-Wilson, C. (1989). ''Flora of Britain and Northern Europe''. yellow toadflax or butter-and-eggs, is a species of flowering plant in the family Plantaginaceae, native to Europe, Siberia and Central Asia. It has also been introduced and is now common in North America. Growth It is a perennial plant with short spreading roots, erect to decumbent stems high, with fine, threadlike, glaucous blue-green leaves long and broad. The flowers are similar to those of the snapdragon, long, pale yellow except for the lower tip which is orange, borne in dense terminal racemes from mid summer to mid autumn. The flowers are mostly visited by bumblebees. The fruit is a globose capsule long and broad, containing numerous small seeds. Ecology The plant is widespread on ruderal spots, along roads, in dunes, and on disturbed and cultivated land. Because the flower is largely closed by its underlip, pollination requires strong insect ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Philip Miller
Philip Miller FRS (1691 – 18 December 1771) was an English botanist and gardener of Scottish descent. Miller was chief gardener at the Chelsea Physic Garden for nearly 50 years from 1722, and wrote the highly popular ''The Gardeners Dictionary''. Life Born in Deptford or Greenwich, Miller was chief gardener at the Chelsea Physic Garden from 1722 until he was pressured to retire shortly before his death. According to the botanist Peter Collinson, who visited the physic garden in July 1764 and recorded his observation in his commonplace books, Miller "has raised the reputation of the Chelsea Garden so much that it excels all the gardens of Europe for its amazing variety of plants of all orders and classes and from all climates..." He wrote ''The Gardener's and Florists Dictionary or a Complete System of Horticulture'' (1724) and ''The Gardener's Dictionary containing the Methods of Cultivating and Improving the Kitchen Fruit and Flower Garden'', which first appeared in 1731 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silver Y
The silver Y (''Autographa gamma'') is a migratory moth of the family Noctuidae which is named for the silvery Y-shaped mark on each of its forewings. Description The silver Y is a medium-sized moth with a wingspan of 30 to 45 mm. The wings are intricately patterned with various shades of brown and grey providing excellent camouflage. In the centre of each forewing there is a silver-coloured mark shaped like a letter Y or a (lower case) Greek letter Gamma. There are several different forms with varying colours depending on the climate in which the larvae grow. Technical description and variation ''P. gamma'' Forewing purplish grey, with darker suffusion in places; the lines pale silvery edged on both sides with dark fuscous, the outer line indented on vein 2 and submedian fold, as in ''circumflexa''; the oblique orbicular and the reniform conversely oblique and constricted in middle, both edged with silvery: the median area below middle blackish, containing a silvery gamm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weichselian Glaciation
The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (german: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (''Weichsel-Kaltzeit''), Weichselian glacial (''Weichsel-Glazial''), ''Weichselian Stage'' or, rarely, the Weichselian complex (''Weichsel-Komplex''). In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strata
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and ''lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoxnian Interglacial
__NOTOC__ The Hoxnian Stage was a middle Pleistocene stage (Pleistocene from million to 11,700 years BP) of the geological history of the British Isles. It was an interglacial which preceded the Wolstonian Stage and followed the Anglian Stage. It is equivalent to Marine Isotope Stage 11 (MIS 11). Marine Isotope Stage 11 started 424,000 years ago and ended 374,000 years ago. Lisiecki, L. E. (2005)Ages of MIS boundaries.http://www.lorraine-lisiecki.com/stack.html LR04 Benthic Stack] Boston University, Boston, MA The Hoxnian is divided into sub-stages Ho I to Ho IV. History The Hoxnian Stage is named after Hoxne in the English county of Suffolk where some of the deposits created were first found. It was identified and dated with palynology or pollen evidence in the biostratigraphy and later updated with aminostratigraphic techniques. Based on stratigraphic information the Hoxnian happened after the Anglian glacial as Anglian soil is frequently found underneath Hoxnian deposits. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stenoptilia Bipunctidactyla
''Stenoptilia bipunctidactyla'', also known as the twin-spot plume is a moth of the Pterophoroidea family found in North Africa, Asia and Europe. It was first described by the Austrian physician and naturalist, Giovanni Antonio Scopoli in 1763. It is one of four similar looking moths. Description The wingspan is 17–25 mm. The moths fly from dusk, in two overlapping generations from March to October, depending on location. They are also attracted to light. ;Similar species This moth may be an aggregate of species with similar looking wings and is part of the ''Stenoptilia bipunctidactyla'' group of four species which all look similar. The other moths of this group are, * small scabious plume ('' Stenoptilia annadactyla'') * scarce plume ('' Stenoptilia inopinata'') * Gregson's plume ('' Stenoptilia scabiodactylus'') ;Early stages The larvae feed on devil's-bit scabious ('' Succisa pratensis''), common toadflax (''Linaria vulgaris''), weasel's snout ('' Misopates orontiu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brown Rustic
The brown rustic (''Rusina ferruginea'') is a species of moth of the family Noctuidae. It is found in Europe. then East across the Palearctic to the Sayan Mountains in Central Asia. The wingspan is 32–40 mm. The ground colour of the forewings is dark brown. A series of small white marks run along the costa. The stigmata are not well defined. The antemedian line runs obliquely from the costa and is darker than the ground colour. The postmedian line is fine and also darker than ground colour. The subterminal line is dark and irregular. The hindwings are yellow brown, with darker veins and a small discal spot. Adult caterpillars are reddish-brown ground. The yellow-white dorsal line is very narrow, as are the clear secondary back lines. The posterior segments of the body have blackish slashes. The lateral stripe is grey-brown, the stigma black and the head dark brown. The moth flies from June to July depending on the location. The larvae feed on various herbaceous plants, i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyrrhia Umbra
''Pyrrhia umbra'', the bordered sallow, is a moth of the family Noctuidae. The species was first described by Johann Siegfried Hufnagel in 1766. It is found in all of Europe, east through Anatolia to Iran, Afghanistan, Pakistan and Nepal and through central Asia to Japan. In mountains it can be found up to elevations of 1,600 meters. Technical description and variation The wingspan is 27–35 mm. The length of the forewings is 16–19 mm. The forewings are a deep olive yellow, faintly dark dusted, from the base to the outer line, beyond which the terminal area is purplish grey, paling towards termen; the lines bright brown; the inner angled inwards on the veins and outwards between them; the outer stronger, oblique and slightly sinuous from the subcostal bend, generally followed by a purplish-grey shade; median shade bent on median vein: submarginal line lunulate-dentate, dark brown, the area beyond it often golden brown; orbicular and reniform of the ground colour, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bog Fritillary
''Boloria eunomia'', the bog fritillary or ocellate bog fritillary, is a butterfly Butterflies are insects in the macrolepidopteran clade Rhopalocera from the Order (biology), order Lepidoptera, which also includes moths. Adult butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. The ... of the family Nymphalidae. Description The length of the forewings is 20–24 mm. The wings are orange brown with dark markings. The color of the hindwings are orangish brown with a tan postmedian band followed by a row of round silver spots. Seitz- ''A. aphirape'' Hbn. (= ''eunomia'' Esp., ''tomyris'' Hbst.) (67f). Above pale reddish yellow, with a narrow black margin and small black submarginal lunules; the basal area separated from the central area by a black dentate line and bearing heavy markings. The median area with but one very regular row of dots in the middle, at the proximal side of which there are often feeble shadows in the female ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falseuncaria Ruficiliana
''Falseuncaria ruficiliana'', the red-fringed conch, is a species of moth of the family Tortricidae. It is found in China (Xinjiang) and most of Europe. The habitat consists of limestone, heathland and moorland. The wingspan is 13–15 mm. It resembles the related species '' Falseuncaria degreyana'', but in this species the forewing's brown cross-band is clearly wider and more marked. The forewings are narrow and evenly-wide, warm reddish-brown, in the middle with a wide, slanted, dark brown cross-band, which usually reaches the front edge. The band is narrowly edged with white on both sides. The outer edge of the wing is slightly darker than the rest. The hindwings are grey-brown and relatively narrow. There are two generations per year, with adults on wing in May and again from July to August. The larvae feed on the seeds of ''Primula veris'', '' Primula farinosa'', ''Linaria vulgaris'', '' Inula officinalis'', '' Aster linosyris'', ''Bellis perennis'', ''Gentiana verna' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Satyr Pug
''Eupithecia satyrata'', the satyr pug, is a species of moth of the family Geometridae. It was described by Jacob Hübner in 1813. It is found from Ireland, through northern and central Europe (from Scandinavia to the northern Mediterranean) east to all of Russia and central Asia and western Siberia to Tibet. It is also present in North Africa and North America. The wingspan is . ''Eupithecia satyrata'' is variable in pattern. The ground colour of the wings is ash grey or brownish. The veins often have a black with white dusting. There are paler crosslines. On the forewings a very indistinct terminal fascia ends in a tiny tornal spot. There is a fine discal spot on the forewing. This is absent on the hindwing. Prout gives an account of the variations.Prout, L. B. (1912–16). Geometridae. In A. Seitz (ed.) ''The Macrolepidoptera of the World''. The Palaearctic Geometridae, 4. 479 pp. Alfred Kernen, Stuttgarpdf */ref> Adults are on wing from March to September. There is one gene ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
