Ancient Greece was a civilization belonging to a period of Greek history from the Greek Dark Ages of the 12th–9th centuries BC to the end of antiquity. Following this period was the beginning of the Early Middle Ages and the Byzantine era. Three centuries after the Late Bronze Age collapse of Mycenaean Greece, Greek urban poleis began to form in the 8th century BC, ushering in the Archaic period and colonization of the Mediterranean Basin; this was followed by the period of Classical Greece, an era that began with the Greco-Persian Wars, lasting from the 5th to 4th centuries BC. Due to the conquests by Alexander the Great of Macedon, Hellenistic civilization flourished from Central Asia to the western end of the Mediterranean Sea; the Hellenistic period came to an end with the conquests and annexations of the eastern Mediterranean world by the Roman Republic, which established the Roman province of Macedonia in Roman Greece, the province of Achaea during the Roman Empire. Classical Greek culture philosophy, had a powerful influence on ancient Rome, which carried a version of it to many parts of the Mediterranean Basin and Europe.
For this reason, Classical Greece is considered to be the seminal culture which provided the foundation of modern Western culture and is considered the cradle of Western civilization. Classical Greek culture gave great importance to knowledge. Science and religion were not separate and getting closer to the truth meant getting closer to the gods. In this context, they understood the importance of mathematics as an instrument for obtaining more reliable knowledge. Greek culture, in a few centuries and with a limited population, managed to explore and make progress in many fields of science, mathematics and knowledge in general. Classical antiquity in the Mediterranean region is considered to have begun in the 8th century BC and ended in the 6th century AD. Classical antiquity in Greece was preceded by the Greek Dark Ages, archaeologically characterised by the protogeometric and geometric styles of designs on pottery. Following the Dark Ages was the Archaic Period, beginning around the 8th century BC.
The Archaic Period saw early developments in Greek culture and society which formed the basis for the Classical Period. After the Archaic Period, the Classical Period in Greece is conventionally considered to have lasted from the Persian invasion of Greece in 480 until the death of Alexander the Great in 323; the period is characterized by a style, considered by observers to be exemplary, i.e. "classical", as shown in the Parthenon, for instance. Politically, the Classical Period was dominated by Athens and the Delian League during the 5th century, but displaced by Spartan hegemony during the early 4th century BC, before power shifted to Thebes and the Boeotian League and to the League of Corinth led by Macedon; this period saw the Greco-Persian Wars and the Rise of Macedon. Following the Classical period was the Hellenistic period, during which Greek culture and power expanded into the Near and Middle East; this period ends with the Roman conquest. Roman Greece is considered to be the period between Roman victory over the Corinthians at the Battle of Corinth in 146 BC and the establishment of Byzantium by Constantine as the capital of the Roman Empire in AD 330.
Late Antiquity refers to the period of Christianization during the 4th to early 6th centuries AD, sometimes taken to be complete with the closure of the Academy of Athens by Justinian I in 529. The historical period of ancient Greece is unique in world history as the first period attested directly in proper historiography, while earlier ancient history or proto-history is known by much more circumstantial evidence, such as annals or king lists, pragmatic epigraphy. Herodotus is known as the "father of history": his Histories are eponymous of the entire field. Written between the 450s and 420s BC, Herodotus' work reaches about a century into the past, discussing 6th century historical figures such as Darius I of Persia, Cambyses II and Psamtik III, alluding to some 8th century ones such as Candaules. Herodotus was succeeded by authors such as Thucydides, Demosthenes and Aristotle. Most of these authors were either Athenian or pro-Athenian, why far more is known about the history and politics of Athens than those of many other cities.
Their scope is further limited by a focus on political and diplomatic history, ignoring economic and social history. In the 8th century BC, Greece began to emerge from the Dark Ages which followed the fall of the Mycenaean civilization. Literacy had been lost and Mycenaean script forgotten, but the Greeks adopted the Phoenician alphabet, modifying it to create the Greek alphabet. Objects with Phoenician writing on them may have been available in Greece from the 9th century BC, but the earliest evidence of Greek writing comes from graffiti on Greek pottery from the mid-8th century. Greece was divided into many small self-governing communities, a pattern dictated by Greek geography: every island and plain is cut off from its neighbors by the sea or mountain ranges; the Lelantine War is the earliest documented war of the ancient Greek period. It was fought between the important poleis of Chalcis and Eretria over the fertile Lelantine plain of Euboea. Both cities seem to have suffered a decline as result of the long war, though Chalcis was the nominal victor.
A mercantile class arose in the first half of the 7th century BC, shown by the introduction of coinage in about 680 BC. This
The leek moth or onion leaf miner is a species of moth of family Acrolepiidae and the genus Acrolepiopsis. The species is native to Europe and Siberia, but is found in North America, where it is an invasive species. While it was recorded in Hawaii, this was a misidentification of Acrolepiopsis sapporensis; the leek moth is similar in appearance to other members of the genus Acrolepiopsis, with mottled brown and white wings. Its wing span is 12 mm across, it is a pest of leek crops, as the larvae feed on several species of Allium by mining into the leaves or bulbs. The shape of the leaf mine is variable, ranging from a corridor to a blotch, can be with or without frass; this leaf mining can occur in the stem. In the case of onions and shallots, the larvae mine into the bulb. In North America, where the moth is an invasive species and has few known natural predators, the species threatens the production and biodiversity of Allium, it has the potential to destroy entire crops; the parasitoid Diadromus pulchellus is used to control the spread of and damage caused by the leek moth in Europe and North America.
The wings are brown mottled with white spots and measure about 12 mm across. High individual variation in wing pattern can make the leek moth difficult to distinguish from other Acrolepiopsis species at first, but its distinct genitalia make it identifiable. Males of this species can be identified by their long saccus, a portion of the male genitalia used for grasping females, females by their long and flat ductus bursae, a portion of the female reproductive tract; the leek moth is native to Europe. Scandinavia and Russia mark the northwestern and northeastern bounds of its range and its presence extends to Algeria in the south, it is an invasive species in North America, where it was first discovered in Canada in 1993. It has since expanded its North American range to include parts of Ontario, Prince Edward Island, New York. Climate models suggest that the leek moth's range could continue to expand to encompass a larger portion of eastern North America; the female leek moth selects the host plant for oviposition.
She is drawn to the plant through chemical attractants released by the plant. Egg-laying does not take place however. Propyl-cysteine-sulfoxide has been shown to induce egg-laying in the leek moth and could be involved in host plant selection as a characteristic signal of Allium. Larvae feed on plants of the genus Allium, including:The leek moth prefers A. sativum, garlic, A. porrum, A. cepa, onion, to other species of Allium. Oviposition takes place in three behavioral stages: slow walking and egg-laying; when given the choice between plants of the same species and of different sizes, females choose to lay their eggs on the larger plant. Development time from egg to adult is variable depending on temperature ranging from 3 weeks at higher temperatures to 6 weeks at lower temperatures; the number of generations possible each year depends on local climate conditions. Whereas three or more generations can be completed in Ontario and Poland, only two can be completed in Sweden. Adults lay eggs within 10 days of adulthood.
Eggs are laid on the leaves of the larval host plant, into which first instar larvae mine and subsequently complete five instars, reaching a length of 13–14 mm when mature. Larvae are light yellow-green in color with a brownish-yellow head. After reaching maturity, fifth instar larvae emerge from the host plant and spin a cocoon, on the host plant or nearby. Cocoons are white in pupa reddish-brown. If daylengths during previous larval stages are shorter than 15 hours, emergent adults will enter diapause to overwinter. Otherwise, adults lay another generation of eggs. Knowledge of the leek moth's natural predators in North America is limited, but several larval and pupal parasitoids of the species have been documented in Europe. Parasitoids lay their eggs within or attached to the body of the host, the parasitoid larvae killing the host. Parasitoids are shown to parasitize the leek moth to a greater extent when leek moth populations are large and in early leek moth generations, suggesting that parasitism is less significant in smaller populations and in generations.
The leek moth is most vulnerable to parasitism in its pupal stage when it is no longer protected by the interior of its host plant. Diadromus pulchellus, a host-specific parasitoid of the leek moth, has been introduced in the Ottawa region in Canada as a biological control method for the invasive moth. During mating, males respond to calling females with the emission of a pheromone containing n-alkanes. Males flutter their wings, which acts to volatilize the pheromone through heat generation and disturb the pheromone molecules; the pheromone acts as an aphrodisiac for the female while inhibiting the sexual behavior of other males. These compounds can be transferred to the female during mating and their sexual inhibitory effects on conspecific males favor the monogamy seen in the leek moth. In eastern Ontario, the leek moth undergoes three flight periods each year; the first flight consists of overwintering adults. The second peaks in early July and consists of first generation adults; the third peaks consists of second generation adults.
This pattern again suggests. Females rely on the olfactory detection of volatile chemoattractants in host plant selec
Sugar is the generic name for sweet-tasting, soluble carbohydrates, many of which are used in food. The various types of sugar are derived from different sources. Simple sugars are called monosaccharides and include glucose and galactose. "Table sugar" or "granulated sugar" refers to a disaccharide of glucose and fructose. In the body, sucrose is hydrolysed into glucose. Sugars are found in the tissues of most plants, but sucrose is concentrated in sugarcane and sugar beet, making them ideal for efficient commercial extraction to make refined sugar. Sugarcane originated in tropical Indian subcontinent and Southeast Asia, is known of from before 6,000 BP, sugar beet was first described in writing by Olivier de Serres and originated in southwestern and Southeast Europe along the Atlantic coasts and the Mediterranean Sea, in North Africa, Macaronesia, to Western Asia. In 2016, the combined world production of those two crops was about two billion tonnes. Other disaccharides include lactose. Longer chains of sugar molecules are called polysaccharides.
Some other chemical substances, such as glycerol and sugar alcohols, may have a sweet taste, but are not classified as sugar. Sucrose is used in prepared foods, is sometimes added to commercially available beverages, may be used by people as a sweetener for foods and beverages; the average person consumes about 24 kilograms of sugar each year, or 33.1 kilograms in developed countries, equivalent to over 260 food calories per day. As sugar consumption grew in the latter part of the 20th century, researchers began to examine whether a diet high in sugar refined sugar, was damaging to human health. Excessive consumption of sugar has been implicated in the onset of obesity, cardiovascular disease and tooth decay. Numerous studies have tried to clarify those implications, but with varying results because of the difficulty of finding populations for use as controls that consume little or no sugar. In 2015, the World Health Organization recommended that adults and children reduce their intake of free sugars to less than 10%, encouraged a reduction to below 5%, of their total energy intake.
The etymology reflects the spread of the commodity. From Sanskrit शर्करा, meaning "ground or candied sugar," "grit, gravel", came Persian shakar, whence Arabic سكر, whence Medieval Latin succarum, whence 12th-century French sucre, whence the English word sugar. Italian zucchero, Spanish azúcar, Portuguese açúcar came directly from Arabic, the Spanish and Portuguese words retaining the Arabic definite article; the earliest Greek word attested is σάκχαρις. The English word jaggery, a coarse brown sugar made from date palm sap or sugarcane juice, has a similar etymological origin: Portuguese jágara from the Malayalam ചക്കരാ, itself from the Sanskrit शर्करा. Sugar has been produced in the Indian subcontinent since ancient times and its cultivation spread from there into modern-day Afghanistan through the Khyber Pass, it was not plentiful or cheap in early times, in most parts of the world, honey was more used for sweetening. People chewed raw sugarcane to extract its sweetness. Sugarcane was a native of Southeast Asia.
Different species seem to have originated from different locations with Saccharum barberi originating in India and S. edule and S. officinarum coming from New Guinea. One of the earliest historical references to sugarcane is in Chinese manuscripts dating to 8th century BCE, which state that the use of sugarcane originated in India. In the tradition of Indian medicine, the sugarcane is known by the name Ikṣu and the sugarcane juice is known as Phāṇita, its varieties and characterics are defined in nighaṇṭus such as the Bhāvaprakāśa. Sugar remained unimportant until the Indians discovered methods of turning sugarcane juice into granulated crystals that were easier to store and to transport. Crystallized sugar was discovered by the time of the Imperial Guptas, around the 5th century CE. In the local Indian language, these crystals were called khanda, the source of the word candy. Indian sailors, who carried clarified butter and sugar as supplies, introduced knowledge of sugar along the various trade routes they travelled.
Traveling Buddhist monks took sugar crystallization methods to China. During the reign of Harsha in North India, Indian envoys in Tang China taught methods of cultivating sugarcane after Emperor Taizong of Tang made known his interest in sugar. China established its first sugarcane plantations in the seventh century. Chinese documents confirm at least two missions to India, initiated in 647 CE, to obtain technology for sugar refining. In the Indian subcontinent, the Middle East and China, sugar became a staple of cooking and desserts. Nearchus, admiral of Alexander of Macedonia, knew of sugar during the year 325 B. C. because of his participation in the campaign of India led by Alexander. The Greek physician Pedanius Dioscorides in the 1st century CE described sugar in his medical treatise De Materia Medica, Pliny the Elder, a 1st-century CE Roman, described sugar in his Natural History: "Sugar is made in Arabia as well, but Indian sugar is better, it is a kind of honey found in cane, white as gum, it crunches between the teeth.
It comes in lumps the size of a hazelnut. Sugar is used only for medical purposes." Crusaders brought sugar back to Europe after their campaigns in the Hol
The onion known as the bulb onion or common onion, is a vegetable, the most cultivated species of the genus Allium. Its close relatives include the garlic, leek and Chinese onion; this genus contains several other species variously referred to as onions and cultivated for food, such as the Japanese bunching onion, the tree onion, the Canada onion. The name "wild onion" is applied to a number of Allium species, but A. cepa is known from cultivation. Its ancestral wild original form is not known, although escapes from cultivation have become established in some regions; the onion is most a biennial or a perennial plant, but is treated as an annual and harvested in its first growing season. The onion plant has a fan of hollow, bluish-green leaves and its bulb at the base of the plant begins to swell when a certain day-length is reached; the bulbs are composed of shortened, underground stems surrounded by fleshy modified scale that envelop a central bud at the tip of the stem. In the autumn, the foliage dies down and the outer layers of the bulb become dry and brittle.
The crop is harvested and dried and the onions are ready for use or storage. The crop is prone to attack by a number of pests and diseases the onion fly, the onion eelworm, various fungi cause rotting; some varieties of A. cepa, such as shallots and potato onions, produce multiple bulbs. Onions are used around the world; as a food item, they are served cooked, as a vegetable or part of a prepared savoury dish, but can be eaten raw or used to make pickles or chutneys. They are pungent when contain certain chemical substances which irritate the eyes; the onion plant known as the bulb onion or common onion, is the most cultivated species of the genus Allium. It was first described by Carl Linnaeus in his 1753 work Species Plantarum. A number of synonyms have appeared in its taxonomic history: Allium cepa var. aggregatum – G. Don Allium cepa var. bulbiferum – Regel Allium cepa var. cepa – Linnaeus Allium cepa var. multiplicans – L. H. Bailey Allium cepa var. proliferum – Regel Allium cepa var. solaninum – Alef Allium cepa var. viviparum – Mansf.
A. Cepa is known from cultivation, but related wild species occur in Central Asia; the most related species include A. vavilovii and A. asarense from Iran. However and Hopf state that "there are doubts whether the A. vavilovii collections tested represent genuine wild material or only feral derivatives of the crop."The vast majority of cultivars of A. cepa belong to the "common onion group" and are referred to as "onions". The Aggregatum group of cultivars includes both shallots and potato onions; the genus Allium contains a number of other species variously referred to as onions and cultivated for food, such as the Japanese bunching onion, Egyptian onion, Canada onion. Cepa is accepted as Latin for "onion" and has an affinity with Ancient Greek: κάπια and Albanian: qepë and is ancestral to Aromanian: tseapã, Catalan: ceba, Occitan: ceba, Spanish: cebolla, Romanian: ceapă; the English word chive is derived from the Old French cive, which derived from cepa. The onion plant has been selectively bred in cultivation for at least 7,000 years.
It is a biennial plant, but is grown as an annual. Modern varieties grow to a height of 15 to 45 cm; the leaves are yellowish - to bluish green and grow alternately in a fan-shaped swathe. They are fleshy and cylindrical, with one flattened side, they are at their broadest about a quarter of the way up, beyond which they taper towards a blunt tip. The base of each leaf is a flattened white sheath that grows out of a basal disc. From the underside of the disc, a bundle of fibrous roots extends for a short way into the soil; as the onion matures, food reserves begin to accumulate in the leaf bases and the bulb of the onion swells. In the autumn, the leaves die back and the outer scales of the bulb become dry and brittle, so the crop is normally harvested. If left in the soil over winter, the growing point in the middle of the bulb begins to develop in the spring. New leaves appear and a long, hollow stem expands, topped by a bract protecting a developing inflorescence; the inflorescence takes the form of a globular umbel of white flowers with parts in sixes.
The seeds are glossy triangular in cross section. The average pH of an onion is around 5.5 Because the wild onion is extinct and ancient records of using onions span western and eastern Asia, the geographic origin of the onion is uncertain, with domestication worldwide. Food uses of onions date back thousands of years in China and Persia. Traces of onions recovered from Bronze Age settlements in China suggest that onions were used as far back as 5000 BCE, not only for their flavour, but the bulb's durability in storage and transport. Ancient Egyptians revered the onion bulb, viewing its spherical shape and concentric rings as symbols of eternal life. Onions were used in Egyptian burials, as evidenced by onion traces found in the eye sockets of Ramesses IV. Pliny the Elder of the first century CE wrote about the use of onions and cabbage in Pompeii, he documented Roman beliefs about the onion's ability to improve ocular ailments, aid in sleep, heal everything from oral sores and toothaches to dog bites and dysentery.
Soil is a mixture of organic matter, gases and organisms that together support life. Earth's body of soil, called the pedosphere, has four important functions: as a medium for plant growth as a means of water storage and purification as a modifier of Earth's atmosphere as a habitat for organismsAll of these functions, in their turn, modify the soil; the pedosphere interfaces with the lithosphere, the hydrosphere, the atmosphere, the biosphere. The term pedolith, used to refer to the soil, translates to ground stone in the sense "fundamental stone". Soil consists of a solid phase of minerals and organic matter, as well as a porous phase that holds gases and water. Accordingly, soil scientists can envisage soils as a three-state system of solids and gases. Soil is a product of several factors: the influence of climate, relief and the soil's parent materials interacting over time, it continually undergoes development by way of numerous physical and biological processes, which include weathering with associated erosion.
Given its complexity and strong internal connectedness, soil ecologists regard soil as an ecosystem. Most soils have a dry bulk density between 1.1 and 1.6 g/cm3, while the soil particle density is much higher, in the range of 2.6 to 2.7 g/cm3. Little of the soil of planet Earth is older than the Pleistocene and none is older than the Cenozoic, although fossilized soils are preserved from as far back as the Archean. Soil science has two basic branches of study: pedology. Edaphology studies the influence of soils on living things. Pedology focuses on the formation and classification of soils in their natural environment. In engineering terms, soil is included in the broader concept of regolith, which includes other loose material that lies above the bedrock, as can be found on the Moon and on other celestial objects as well. Soil is commonly referred to as earth or dirt. Soil is a major component of the Earth's ecosystem; the world's ecosystems are impacted in far-reaching ways by the processes carried out in the soil, from ozone depletion and global warming to rainforest destruction and water pollution.
With respect to Earth's carbon cycle, soil is an important carbon reservoir, it is one of the most reactive to human disturbance and climate change. As the planet warms, it has been predicted that soils will add carbon dioxide to the atmosphere due to increased biological activity at higher temperatures, a positive feedback; this prediction has, been questioned on consideration of more recent knowledge on soil carbon turnover. Soil acts as an engineering medium, a habitat for soil organisms, a recycling system for nutrients and organic wastes, a regulator of water quality, a modifier of atmospheric composition, a medium for plant growth, making it a critically important provider of ecosystem services. Since soil has a tremendous range of available niches and habitats, it contains most of the Earth's genetic diversity. A gram of soil can contain billions of organisms, belonging to thousands of species microbial and in the main still unexplored. Soil has a mean prokaryotic density of 108 organisms per gram, whereas the ocean has no more than 107 procaryotic organisms per milliliter of seawater.
Organic carbon held in soil is returned to the atmosphere through the process of respiration carried out by heterotrophic organisms, but a substantial part is retained in the soil in the form of soil organic matter. Since plant roots need oxygen, ventilation is an important characteristic of soil; this ventilation can be accomplished via networks of interconnected soil pores, which absorb and hold rainwater making it available for uptake by plants. Since plants require a nearly continuous supply of water, but most regions receive sporadic rainfall, the water-holding capacity of soils is vital for plant survival. Soils can remove impurities, kill disease agents, degrade contaminants, this latter property being called natural attenuation. Soils maintain a net absorption of oxygen and methane and undergo a net release of carbon dioxide and nitrous oxide. Soils offer plants physical support, water, temperature moderation and protection from toxins. Soils provide available nutrients to plants and animals by converting dead organic matter into various nutrient forms.
A typical soil is about 50% solids, 50% voids of which half is occupied by water and half by gas. The percent soil mineral and organic content can be treated as a constant, while the percent soil water and gas content is considered variable whereby a rise in one is balanced by a reduction in the other; the pore space allows for the infiltration and movement of air and water, both of which are critical for life existing in soil. Compaction, a common problem with soils, reduces this space, preventing air and water from reaching plant roots and soil organisms. Given sufficient time, an undifferentiated soil will evolve a soil profile which consists of two or more layers, referred to as soil horizons, that differ in one or more properties such as in their texture, density, consistency, temperature and reactivity; the horizons differ in thickness and gene
In scientific nomenclature, a synonym is a scientific name that applies to a taxon that goes by a different scientific name, although the term is used somewhat differently in the zoological code of nomenclature. For example, Linnaeus was the first to give a scientific name to the Norway spruce, which he called Pinus abies; this name is no longer in use: it is now a synonym of the current scientific name, Picea abies. Unlike synonyms in other contexts, in taxonomy a synonym is not interchangeable with the name of which it is a synonym. In taxonomy, synonyms have a different status. For any taxon with a particular circumscription and rank, only one scientific name is considered to be the correct one at any given time. A synonym cannot exist in isolation: it is always an alternative to a different scientific name. Given that the correct name of a taxon depends on the taxonomic viewpoint used a name, one taxonomist's synonym may be another taxonomist's correct name. Synonyms may arise whenever the same taxon is named more than once, independently.
They may arise when existing taxa are changed, as when two taxa are joined to become one, a species is moved to a different genus, a variety is moved to a different species, etc. Synonyms come about when the codes of nomenclature change, so that older names are no longer acceptable. To the general user of scientific names, in fields such as agriculture, ecology, general science, etc. A synonym is a name, used as the correct scientific name but, displaced by another scientific name, now regarded as correct, thus Oxford Dictionaries Online defines the term as "a taxonomic name which has the same application as another one, superseded and is no longer valid." In handbooks and general texts, it is useful to have synonyms mentioned as such after the current scientific name, so as to avoid confusion. For example, if the much advertised name change should go through and the scientific name of the fruit fly were changed to Sophophora melanogaster, it would be helpful if any mention of this name was accompanied by "".
Synonyms used in this way may not always meet the strict definitions of the term "synonym" in the formal rules of nomenclature which govern scientific names. Changes of scientific name have two causes: they may be taxonomic or nomenclatural. A name change may be caused by changes in the circumscription, position or rank of a taxon, representing a change in taxonomic, scientific insight. A name change may be due to purely nomenclatural reasons, that is, based on the rules of nomenclature. Speaking in general, name changes for nomenclatural reasons have become less frequent over time as the rules of nomenclature allow for names to be conserved, so as to promote stability of scientific names. In zoological nomenclature, codified in the International Code of Zoological Nomenclature, synonyms are different scientific names of the same taxonomic rank that pertain to that same taxon. For example, a particular species could, over time, have had two or more species-rank names published for it, while the same is applicable at higher ranks such as genera, orders, etc.
In each case, the earliest published name is called the senior synonym, while the name is the junior synonym. In the case where two names for the same taxon have been published the valid name is selected accorded to the principle of the first reviser such that, for example, of the names Strix scandiaca and Strix noctua, both published by Linnaeus in the same work at the same date for the taxon now determined to be the snowy owl, the epithet scandiaca has been selected as the valid name, with noctua becoming the junior synonym. One basic principle of zoological nomenclature is that the earliest published name, the senior synonym, by default takes precedence in naming rights and therefore, unless other restrictions interfere, must be used for the taxon. However, junior synonyms are still important to document, because if the earliest name cannot be used the next available junior synonym must be used for the taxon. For other purposes, if a researcher is interested in consulting or compiling all known information regarding a taxon, some of this may well have been published under names now regarded as outdated and so it is again useful to know a list of historic synonyms which may have been used for a given current taxon name.
Objective synonyms refer to taxa with same rank. This may be species-group taxa of the same rank with the same type specimen, genus-group taxa of the same rank with the same type species or if their type species are themselves objective synonyms, of family-group taxa with the same type genus, etc. In the case of subjective synonyms, there is no such shared type, so the synonymy is open to taxonomic judgement, meaning that th
The Castelltallat range is located in central Catalonia between the counties of Bages and Solsonès, extending over the provinces of Barcelona and Lleida, occupying an area of about 65 square kilometres. It is one of the isolated hills of the Catalan Central Depression and is located at its southwestern end. Geologically the Castelltallat range is made up of limestone and marl mountains oriented WSW-ENE; the highest point of the range is the 936 m high "Tossal". The northern slopes are steep and forested, while the southern slopes are used for agriculture owing to their lesser inclination. Most of the mountain belongs to the municipality of Sant Mateu de Bages while the western part lies within the municipalities of Pinós and La Molsosa; the village of Castelltallat was a municipality until 1840 when it became part of San Mateu de Bages municipal term. The parish church of Sant Miquel has been documented since 1031 and is located at an altitude of 887 m; the Church contains samples of Romanesque, Renaissance and neoclassical architectural styles.
It was built at the feet of the now ruined 10th or 11th century Castelltallat castle which gave its name to the mountain range, for "Castell talaiat" comes from the words "Castell", "Talaia", watchtower. Submediterranean climate with a mean annual temperature of 12°C, January is the coldest month and July and August the warmest and annual precipitation of about 600 liters with little or no snow. Most of the range is part of an "Areas of Natural Interest Plan" of the government of Catalonia. Before the wildfires of 1994 and 1998, pines dominated the landscape: Pinus nigra, Pinus halepensis Pinus sylvestris and a lesser extent Pinus pinea. After the fires Quercus humilis and Quercus ilex sprouts became the most visible trees. Where there is no forest predominate meadow Aphyllantion or Brachypodium and shrubs specially Dorycnum pentaphyllum and rosemary, it is remarkable the presence of he gypsophylous plant named ruac in some small gypsum patchs and the bastard balm. Interesting are the examples of yellow foxglove and the broom.
The bird population seems to have been little affected by wildfires. Among the birds Eurasian eagle-owl is the greatest between the nesting birds. Since a few years it can see the griffon vulture fly, coming from the neighboring county of upper Solsonès; the number of partridges do not seem to have changed after wildfires. Between feral mammals the number of wild boars and foxes is increasing; the population of rabbits in contrast, is variable. The astronomical observatory was built close to the ruins of the ancient castle as part of the revitalization of the area after numerous forest fires. Opened in 2004, the dome of the observatory has a diameter of 5 meters and the telescope 400 mm. Catalan Central Depression Gran Enciclopèdia Catalana Panareda Clopés, Josep Maria. Guia de Catalunya, Barcelona:Caixa de Catalunya. ISBN 84-87135-01-3. ISBN 84-87135-02-1 Arqueociencia with picture of the castle ruins. Castelltallat observatory and Turistic information with pictures Statistical information - Institut d'Estadística de Catalunya