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Friday, September 12, 2014

Whale

Whale

From Wikipedia, the free encyclopedia

Whale
Temporal range: 50–0Ma
O
S
D
C
P
T
J
K
N
Eocene – Recent
Eubalaena glacialis with calf.jpg
North Atlantic right whales, mother and calf
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Subclass: Eutheria
Order: Cetacea

Whale (origin Old English hwæl from Proto-Germanic *hwalaz) is the common name for various marine mammals of the order Cetacea.[1] The term whale sometimes refers to all cetaceans, but more often it excludes dolphins and porpoises, which belong to the suborder Odontoceti (toothed whales). This suborder includes the sperm whale, killer whale, pilot whale, and beluga whale. The other Cetacean suborder, Mysticeti (baleen whales), comprises filter feeders that eat small organisms caught by straining seawater through a comblike structure found in the mouth called baleen. This suborder includes the blue whale, the humpback whale, the bowhead whale and the minke whale. All cetaceans have forelimbs modified as fins, a tail with horizontal flukes, and nasal openings (blowholes) on top of the head.

Whales range in size from the blue whale, the largest animal known to have ever existed[2] at 30 m (98 ft) and 180 tonnes (180 long tons; 200 short tons), to pygmy species such as the pygmy sperm whale at 3.5 m (11 ft). Whales inhabit all the world's oceans and number in the millions, with annual population growth rate estimates for various species ranging from 3% to 13%.[3] Whales are long-lived, humpback whales living for up to 77 years, while bowhead whales may live for over a century.

Human hunting of whales from the 17th century until 1986 radically reduced the populations of some whale species. Whales have appeared in literature since the time of the Old Testament, play a role in Inuit creation myths, and are revered by coastal people in Ghana and Vietnam.

Taxonomy

Cetaceans are divided into two suborders:
  • The largest suborder, Mysticeti (baleen whales), is characterized by baleen, a sieve-like structure in the upper jaw made of keratin, which it uses to filter plankton from the water.
  • Odontoceti (toothed whales) bear sharp teeth for hunting. Odontoceti includes dolphins and porpoises, which means that if they are considered not to be whales, the informal grouping 'whale' is not a clade.
Cetaceans and artiodactyls are now classified under the super-order Cetartiodactyla, which includes both whales and hippopotami. Whales are the hippopotamus's closest living relatives.[4]

Evolution

Ambulocetus natans – a primitive cetacean

All cetaceans, including whales, dolphins and porpoises, are descendants of land-dwelling mammals of the Artiodactyl order (even-toed ungulates). Both are related to the Indohyus, an extinct semi-aquatic deer-like ungulate, from which they split around 54 million years ago.[5][6] These primitive cetaceans first took to the sea about 50 million years ago and became fully aquatic about 5–10 million years later.[7] Their features became adapted for living in the marine environment. Major anatomical changes include streamlining of the body, the migration of the nasal openings towards the top of the cranium, the shrinking and eventual disappearance of the hind limbs, the modification of the forelimbs into flippers, and the growth of flukes on the tail.

Anatomy

Like all mammals, whales breathe air, are warm-blooded, nurse their young with milk from mammary glands, and have body hair.[8] Beneath the skin lies a layer of fat called blubber, which stores energy and insulates the body. Whales have a spinal column, a vestigial pelvic bone, and a four-chambered heart. The neck vertebrae are typically fused, trading flexibility for stability during swimming.[9][10]

Blowhole(s)

Features of a blue whale

Whales breathe via blowholes; baleen whales have two and toothed whales have one. These are located on the top of the head, allowing the animal to remain almost completely submerged while breathing. Breathing involves expelling stale air (which is warm and moist), as well as some mucus and excess water from the blowhole, forming an upward, steamy spout, followed by inhaling fresh air into the lungs.[11] Spout shapes differ among species and help with identification.

Appendages

The body shape is fusiform and the modified forelimbs, or fins, are paddle-shaped. The end of the tail is composed of two flukes, which propel the animal by vertical movement, as opposed to the horizontal movement of a fish tail. Although whales do not possess fully developed hind limbs, some (such as sperm whales and baleen whales) possess discrete rudimentary appendages, which may have feet and digits. Most species have a dorsal fin.[12][13]

In March 2014 in Japan a bottle-nosed dolphin with hind fins about as big as a man's hands, was captured.[14]

Dentition

Toothed whales, such as the sperm whale, possess teeth with cementum cells overlying dentine cells.
Unlike human teeth, which are composed mostly of enamel on the portion of the tooth outside of the gum, whale teeth have cementum outside the gum. Only in larger whales, where the cementum is worn away on the tip of the tooth, does enamel show.[15]

Instead of teeth, baleen whales have a row of baleen plates on the upper side of their jaws that resemble the teeth of a comb.

Ears

The whale ear has specific adaptations to the marine environment. In humans, the middle ear works as an impedance matcher between the outside air's low impedance and the cochlear fluid's high impedance. However, in aquatic mammals, such as whales, there is no great difference between the outer and inner environments. Instead of sound passing through the outer ear to the middle ear, whales receive sound through the throat, from which it passes through a low-impedance fat-filled cavity to the inner ear.[16] The whale ear is acoustically isolated from the skull by air-filled sinus pockets, which allow for greater directional hearing underwater.[17]

Life history and behavior

Reproduction

Males are called 'bulls', females, 'cows' and newborns, 'calves'. Most species do not maintain fixed partnerships and females have several mates each season.[18][19]
The female usually delivers a single calf, which is birthed tail-first to minimize the risk of drowning. Whale cows nurse by actively squirting milk into the mouths of their young. This milk is so rich in fat that it has the consistency of toothpaste.[18] In many species, nursing continues for more than a year and is associated with a strong bond between mother and calf. Reproductive maturity typically occurs at seven to ten years. This mode of reproduction produces few offspring, but increases the survival probability of each one.

Socialization

Whales are known to teach, learn, cooperate, scheme, and even grieve.[20] The neocortex of many species of whale is home to elongated spindle neurons that, prior to 2007, were known only in hominids.[21] In humans these cells are involved in social conduct, emotions, judgment, and theory of mind.[22] Whale spindle neurons are found in areas of the brain that are homologous to where they are found in humans, suggesting that they perform a similar function.[23]

Sleep

Photo of humpback whale with most of its body out of the water and its pectoral fins extended
A humpback whale breaching.

Unlike most animals, whales are conscious breathers. All mammals sleep, but whales cannot afford to become unconscious for long because they may drown. While knowledge of sleep in wild cetaceans is limited, toothed cetaceans in captivity have been recorded to sleep with one side of their brain at a time, ostensibly so that they may swim, breathe consciously, avoid predators and social contact during their period of rest. It is thought that only one hemisphere of the whale's brain sleeps at a time, so that they rest but are never completely asleep.[24]

A 2008 study found that wild sperm whales (Physeter macrocephalus) sleep in vertical postures just under the surface in passive shallow 'drift-dives', generally during the day, during which whales do not respond to passing vessels unless they are in contact, leading to the suggestion that whales possibly sleep during such dives.[25]

Surfacing behavior

Many whales exhibit behaviors that expose large parts of their bodies to the air, such as breaching and tail slapping.

Sounding

Sounding is a term used for whales diving. It is typically only used for longer dives. Whales typically stay close to the surface for a series of short, shallow dives while building their oxygen reserves. They then have a sounding dive.

Lifespan

Whale lifespans vary among species and are not well characterized. Whaling left few older individuals to observe directly. R.M. Nowak of Johns Hopkins University estimated that humpback whales may live as long as 77 years.[26] In 2007, a 19th-century lance fragment was found in a bowhead whale off Alaska, suggesting the individual could be between 115 and 130 years old.[27] Aspartic acid racemization in the whale eye, combined with a harpoon fragment, indicated an age of 211 years for another male, which, if true, would make bowheads the longest-lived extant mammal species.[28][29] The accuracy of this technique has been questioned because racemization does not correlate well with other dating methods.[30]

Vocalization

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Recording of Humpback Whales singing and Clicking.

Problems playing this file? See media help.

Some species, such as the humpback whale, communicate using melodic sounds, known as whale song. These sounds can be extremely loud, depending on the species. Sperm whales have only been heard making clicks, while toothed whales (Odontoceti) use echolocation that can generate about 20,000 watts of sound (+73 dBm or +43 dBw[31]) and be heard for many miles. Whale vocalization is likely to serve many purposes, including echolocation, mating, and identification.[32]

Captive whales have occasionally been known to mimic human speech. Scientists have suggested this indicates a strong desire on behalf of the whales to communicate with humans, as whales have a very different vocal mechanism, so producing human speech likely takes considerable effort.[33]

Ecology

"Whale pump" - the role played by whales in nutrient recycling in the oceans.

Whales are considered as "marine ecosystem engineers" for the following reasons:[34]
  • Whales are major consumers of fish and oceanic invertebrates.
  • Whales act as reservoirs of nutrients, such as iron and nitrogen, and recycle them both horizontally and vertically in the water column.
  • Whale detritus provides energy and habitat for deep sea organisms.

Feeding

Whales are generally classed as predators, but their food ranges from microscopic plankton to very large animals.

Toothed whales eat fish and squid, which they hunt by the use of echolocation. Killer whales sometimes eat other marine mammals, including whales.

Baleen whales, such as humpbacks and blues, mainly eat krill when feeding in the higher latitudes (such as the Southern Ocean). They imbibe enormous amounts of seawater, which they expel through their baleen plates; the krill is retained on the plates and then swallowed.[18] Whales do not drink seawater but indirectly extract water from their food by metabolizing fat.[18]

Whale pump

A 2010 study considered whales to be a positive influence to the productivity of ocean fisheries, in what has been termed a "whale pump." Whales carry nutrients such as nitrogen from the depths back to the surface. This functions as an upward biological pump, reversing an earlier assumption that whales accelerate the loss of nutrients to the bottom. This nitrogen input in the Gulf of Maine is "more than the input of all rivers combined", some 23,000 metric tons each year.[35][36]

Whale fall

Whale carcasses fall to the deep ocean and being massive, with body weights of the range 30 to 160 tonnes (30,000 to 160,000 kg), provide a substantial habitat for marine creatures. Evidence of whale falls in present day and fossil records shows that deep sea whale falls support a rich assemblage of creatures, with a global diversity of 407 species as per Smith & Baco (2003), comparable to other neritic biodiversity hotspots, such as cold seeps and hydrothermal vents.[37]
Deterioration of whale carcasses happens though a series of three stages. Initially, moving organisms such as sharks and hagfish, scavenge the soft tissues at a rapid rate over a period of months, and as long as two years. This is followed by the colonisation of bones and surrounding sediments (which contain organic matter) by enrichment opportunists, such as crustaceans and polychaetes over a period of years. Finally, sulfophilic bacteria reduce the bones releasing hydrogen sulfide enabling the growth of chemoautotrophic organisms, which in turn support other organisms such as mussels, clams, limpets and sea snails. This stage can last for decades and supports rich assemblage of species, averaging 185 species per site as per Smith & Baco (2003).[37]

Interaction with humans

Whaling

Dutch whalers near Spitsbergen. Abraham Storck, 1690
Map showing IWC non-members such as Canada and most Middle Eastern and African countries in white
World map of International Whaling Commission (IWC) members/non-members(member countries in blue)
Diagram showing the pre-whaling of 275,000, 1930's population of 30–40,000, mid-60's population of 650–2,000 and 1994 population of less than 5,000
World population graph of blue whales (Balaenoptera musculus)

Some species of large whales are listed as endangered by multinational organizations, such as CITES, as well as governments and advocacy groups; this is primarily due to the impact of whaling. Whales have been hunted commercially for whale oil, meat, baleen and ambergris (a perfume ingredient from the intestine of sperm whales) since the 17th century.[38] More than 2 million were taken in the 20th century,[39] and by the middle of the century, many populations were severely depleted.

The International Whaling Commission banned commercial whaling in 1986.[40] The ban is not absolute, however, and some whaling continues under the auspices of scientific research[40] (sometimes not proved[41]) or aboriginal rights; current whaling nations are Norway, Iceland and Japan and the aboriginal communities of Siberia, Alaska and northern Canada.

Bycatch

Several species of small whales are caught as bycatch in fisheries for other species. In the Eastern Tropical Pacific tuna fishery, thousands of dolphins drowned in purse-seine nets, until preventive measures were introduced. Gear and deployment modifications, and eco-labelling (dolphin-safe or dolphin-friendly brands of tuna), have contributed to a reduction in dolphin mortality by tuna vessels.[42]

Naval sonar

Environmentalists speculate that advanced naval sonar endangers some cetaceans, including whales. In 2003, British and Spanish scientists suggested in Nature that the effects of sonar trigger whale beachings and to signs that such whales have experienced decompression sickness.[43] Responses in Nature the following year discounted the explanation.[44]
Mass beachings occur in many species, mostly beaked whales that use echolocation for deep diving. The frequency and size of beachings around the world, recorded over the last 1,000 years in religious tracts and more recently in scientific surveys, have been used to estimate the population of various whale species by assuming that the proportion of the total whale population beaching in any one year is constant. Beached whales can give other clues about population conditions, especially health problems. For example, bleeding around ears, internal lesions, and nitrogen bubbles in organ tissue suggest decompression sickness.[20]

Following public concern, the U.S. Defense department was ordered by the 9th Circuit Court to strictly limit use of its Low Frequency Active Sonar during peacetime. Attempts by the UK-based Whale and Dolphin Conservation Society to obtain a public inquiry into the possible dangers of the Royal Navy's equivalent (the "2087" sonar launched in December 2004) failed as of 2008. The European Parliament has requested that EU members refrain from using the powerful sonar system until an environmental impact study has been carried out.

Human mythology

Whale weather-vane atop the Nantucket Historical Association Whaling Museum displaying a sperm whale.

Whales were little understood for most of human history as they spend up to 90% of their lives underwater, only surfacing briefly to breathe.[45] Many cultures, even those that have hunted them, hold whales in awe and feature them in their mythologies.

In China, Yu-kiang, a whale with the hands and feet of a man was said to rule the ocean.[46]

In the Tyrol region of Austria, it was said that if a sunbeam were to fall on a maiden entering womanhood, she would be carried away in the belly of a whale.[47]

Paikea, the youngest and favourite son of the chief Uenuku from the island of Mangaia, in the present day Cook Islands, was said by the Kati Kuri people of Kaikoura to have come from the Pacific Islands on the back of a whale many centuries before.[48]

The whale features in Inuit creation myths. When 'Big Raven', a deity in human form, found a stranded whale, he was told by the Great Spirit where to find special mushrooms that would give him the strength to drag the whale back to the sea and thus return order to the world.[46]

The Tlingit people of northern Canada said that the Orcas were created when the hunter Natsihlane carved eight fish from yellow cedar, sang his most powerful spirit song and commanded the fish to leap into the water.[49]

In Icelandic legend a man threw a stone at a fin whale and hit the blowhole, causing the whale to burst. The man was told not to go to sea for twenty years, but in the nineteenth year he went fishing and a whale came and killed him.[50]

In East African legend, King Sulemani asked God that he might permit him to feed all the beings on earth. A whale came and ate until there was no corn left and then told Sulemani that he was still hungry and that there were 70,000 more in his tribe. Sulemani then prayed to God for forgiveness and thanked the creature for teaching him a lesson in humility.[46]

Some cultures associate divinity with whales, such as among Ghanaians and Vietnamese, who occasionally hold funerals for beached whales, a throwback to Vietnam's ancient sea-based Austro-Asiatic culture.[51][52][53][54]

The Bible mentions whales in Genesis 1:21, Job 7:12, Ezekiel and 32:2. The "sea monsters" in Lamentations 4:3 have been taken by some commentators to refer to marine mammals, in particular whales, although most modern versions use the word "jackals" instead.[55] The story of Jonah being swallowed by a "big Fish" is told both in the Qur'an[56] and in the Bible. The Old Testament contains the Book of Jonah and in the New Testament, Jesus mentions this story in Matthew 12:40.[57]
The engraving by William van der Gouwen shows a 20 m (65.6 ft) long whale, stranded on the Dutch coast between Scheveningen and Katwijk on 3 February 1598.

The 1851 American novel, Moby-Dick by Herman Melville concerns a vexed captain's hunt for a gigantic white whale. Rudyard Kipling's 1902 Just So Stories includes the tale of "How the Whale got his Throat".[58] The film Whale Rider directed by Niki Caro has a Maori girl ride a whale in her quest to be a suitable heir to the chiefship.[59] An enormous whale called Monstro is the final antagonist featured in Walt Disney's 1940 animated film Pinocchio.

And God Created Great Whales, written in 1970 by American composer Alan Hovhaness, is a work for orchestra and whale songs including the recorded sounds of humpback, bowhead, and killer whales.[60] The song "Il n'y a plus rien", from French singer-songwriter Léo Ferré's eponymous album (1973), is an example of biomusic that begins and ends with recorded whale songs mixed with a symphonic orchestra and his voice talking over. Recorded whale song is used in the Missa_Gaia/Earth_Mass by Paul Winter (1982) which is performed at the Cathedral of Saint John the Divine each year to celebrate the Feast of St. Francis. The Sanctus and Benedictus portion uses a four note motif derived from humpback whale song to open and close that segment of the work.[61]

Lake Baikal

Lake Baikal

From Wikipedia, the free encyclopedia

Lake Baikal
Olkhon Island and Lake Baikal.jpg
Karte baikal2.png
Location Siberia, Russia
Coordinates 53°30′N 108°0′ECoordinates: 53°30′N 108°0′E
Lake type Continental rift lake
Primary inflows Selenge, Barguzin, Upper Angara
Primary outflows Angara
Catchment area 560,000 km2 (216,000 sq mi)
Basin countries Russia and Mongolia

Max. length 636 km (395 mi)
Max. width 79 km (49 mi)
Surface area 31,722 km2 (12,248 sq mi)[1]
Average depth 744.4 m (2,442 ft)[1]
Max. depth 1,642 m (5,387 ft)[1]
Water volume 23,615.39 km3 (5,700 cu mi)[1]
Residence time 330 years[2]
Shore length1 2,100 km (1,300 mi)
Surface elevation 455.5 m (1,494 ft)

Frozen January–May
Islands 27 (Olkhon)
Settlements Irkutsk
1 Shore length is not a well-defined measure.

Lake Baikal (Russian: о́зеро Байка́л, tr. Ozero Baykal; IPA: [ˈozʲɪrə bɐjˈkal]; Buryat: Байгал нуур, Mongolian: Байгал нуур, Baygal nuur, meaning "nature lake";[3]) is a rift lake in the south of the Russian region of Siberia, between the Irkutsk Oblast to the northwest and the Buryat Republic to the southeast.

Lake Baikal is the freshwater lake with greatest volume in the world, containing roughly 20% of the world's unfrozen surface fresh water,[4][5] and at 1,642 m (5,387 ft),[1] the deepest.[6] It is also among the clearest[7] of all lakes, and thought to be the world's oldest lake[8] at 25 million years.[9] It is the seventh-largest lake in the world by surface area.

Like Lake Tanganyika, Lake Baikal was formed as an ancient rift valley, having the typical long crescent shape with a surface area of 31,722 km2 (12,248 sq mi). Baikal is home to more than 1,700 species of plants and animals, two-thirds of which can be found nowhere else in the world[10] and was declared a UNESCO World Heritage Site in 1996.[11] It is also home to Buryat tribes who reside on the eastern side of Lake Baikal,[12][13] rearing goats, camels, cattle, and sheep,[13] where the mean temperature varies from a winter minimum of −19 °C (−2 °F) to a summer maximum of 14 °C (57 °F).[14] (As these are mean temperatures of days and nights combined, winter nights are considerably colder and summer days are considerably hotter.)

Geography and hydrography

A digital elevation model of Lake Baikal region
The Yenisei River basin, which includes Lake Baikal

Lake Baikal is in a rift valley, created by the Baikal Rift Zone, where the Earth's crust pulls apart.[5] At 636 km (395 mi) long and 79 km (49 mi) wide, Lake Baikal has the largest surface area of any freshwater lake in Asia, at 31,722 km2 (12,248 sq mi), and is the deepest lake in the world at 1,642 m (5,387 ft). The bottom of the lake is 1,186.5 m (3,893 ft) below sea level, but below this lies some 7 km (4.3 mi) of sediment, placing the rift floor some 8–11 km (5.0–6.8 mi) below the surface: the deepest continental rift on Earth.[5] In geological terms, the rift is young and active—it widens about two cm per year. The fault zone is also seismically active; there are hot springs in the area and notable earthquakes every few years. The lake is divided into three basins: North, Central, and South, with depths of about 900 m (3,000 ft), 1,600 m (5,200 ft), and 1,400 m (4,600 ft), respectively. Fault-controlled accommodation zones rising to depths of about 300 m (980 ft) separate the basins. The North and Central basins are separated by Academician Ridge while the area around the Selenga Delta and the Buguldeika Saddle separates the Central and South basins. The lake drains into the Angara tributary of the Yenisei. Notable landforms include Cape Ryty on Baikal's northwest coast.

Baikal's age is estimated at 25–30 million years, making it one of the most ancient lakes in geological history.[citation needed] It is unique among large, high-latitude lakes, in that its sediments have not been scoured by overriding continental ice sheets. U.S. and Russian studies of core sediment in the 1990s provide a detailed record of climatic variation over the past 250,000 years. Longer and deeper sediment cores are expected in the near future. Lake Baikal is the only confined freshwater lake in which direct and indirect evidence of gas hydrates exists.[15][16][17]

The lake is completely surrounded by mountains. The Baikal Mountains on the north shore and the taiga are technically protected as a national park. It contains 27 islands; the largest, Olkhon, is 72 km (45 mi) long and is the third-largest lake-bound island in the world. The lake is fed by as many as 330 inflowing rivers.[4] The main ones draining directly into Baikal are the Selenga River, the Barguzin River, the Upper Angara River, the Turka River, the Sarma River, and the Snezhnaya River. It is drained through a single outlet, the Angara River.

Despite its great depth, the lake's waters are well-mixed and well-oxygenated throughout the water column, compared to the stratification that occurs in such bodies of water as Lake Tanganyika and the Black Sea.

Wildlife and vegetation

The Baikal seal is endemic to Lake Baikal

Lake Baikal is rich in biodiversity. It hosts more than 1,000 species of plants and 2,500 species of animals based on current knowledge, but the actual figures for both groups are believed to be significantly higher.[18][19] More than 80% of the animals are endemic (found only at Lake Baikal).[19] The Baikal seal or nerpa (Pusa sibirica) is found throughout Lake Baikal.[20] It is one of only three entirely freshwater seal populations in the world, the other two being subspecies of ringed seal.

The watershed of Lake Baikal has numerous flora species represented. The marsh thistle, Cirsium palustre, is found here at the eastern limit of its geographic range.[21]

Fish

Two species of grayling (Thymallus baikalensis and T. brevipinnis) are found only in Baikal and river that drain into the lake.[22][23]

In total there are less than 60 native fish species in the lake, but more than half of these are endemic.[18] The families Abyssocottidae (deep-water sculpins), Comephoridae (golomyankas or Baikal oilfish) and Cottocomephoridae (Baikal sculpins), and the subfamily Cottinae (part of the cottid family) are entirely restricted to the lake basin.[18] All these are part of Cottoidea. Of particular note are the two species of golomyanka (Comephorus baicalensis and C. dybowskii). These long-finned, translucent fish typically live in open water in depths of 100–500 m (330–1,640 ft), but occur both shallower and much deeper. They are the primary prey of the Baikal seal and represent the largest fish biomass in the lake.[24] Beyond members of Cottoidea, there are few endemic fish species in the lake.[18]

The most important local species for fisheries is the omul (Coregonus migratorius), an endemic whitefish.[18] It is caught, smoked and then sold widely in markets around the lake. There is also a second endemic whitefish in the lake, C. baicalensis.[25] The Baikal black grayling (Thymallus baicalensis), Baikal white grayling (T. brevipinnis) and the Baikal sturgeon (Acipenser baerri baicalensis) are other important species with commercial value. They are also endemic to the Lake Baikal basin.[22][23][26][27]

Invertebrates

The lake hosts rich endemic fauna of invertebrates. Epischura baikalensis is endemic to Lake Baikal and the dominating zooplankton species there, making up 80 to 90% of total biomass.[28]

Among the most diverse invertebrate groups are the turbellarian worms, freshwater snails, and amphipod crustaceans.

There are more than 350 species and subspecies of amphipods in the lake and all are endemic.[19] They are exceptionally diverse in ecology and appearance, ranging from the pelagic Macrohectopus to the relatively large deep-water Abyssogammarus and Garjajewia, the tiny herbivorous Micruropus, and the parasitic Brandtia (parasite of lubomirskiid sponges such as Lubomirskia baicalensis) and Pachyschesis (parasitic on other amphipods).[29] The "gigantism" of some Baikal amphipods, which has been compared to that seen in Antarctic amphipods, has been linked to the high level of dissolved oxygen in the lake.[30] Among the "giants" are several species of spiny Acanthogammarus that are found at both shallow and large depths.[31] These conspicuous and common amphipods are essentially carnivores (will also take detritus), and can reach a body length of up to 7 cm (2.8 in).[29][31]

As of 2006, almost 150 freshwater snails are known from Lake Baikal, including 117 endemic species from the subfamilies Baicaliinae (part of Amnicolidae) and Benedictiinae (part of Lithoglyphidae), and the families Planorbidae and Valvatidae.[32] All endemics have been recorded between 20 and 30 m (66 and 98 ft), but the majority mainly live at shallower depths.[32] About 30 freshwater snail species can be seen deeper than 100 m (330 ft), which represents the approximate limit of the sunlight zone, but only 10 are truly deep water species.[32] In general, Baikal snails are thin-shelled and small. Two of the most common species are Benedictia baicalensis and Megalovalvata baicalensis.[33] Bivalve diversity is lower with more than 30 species; about half of these, all in the families Euglesidae, Pisidiidae and Sphaeriidae, are endemic (the only other family in the lake is Unionidae with a single non-endemic species).[33][34] The endemic bivalves are mainly found in shallow depths, with few species from deep water.[35]

With almost 200 described species, including more than 160 endemics, the center of diversity for aquatic freshwater oligochaetes is Lake Baikal.[36] A smaller number of other freshwater annelids are known the lake: 13 species of Hirudinea (leeches) and 4 polychaetes.[36] Several hundred species of nematodes are known from the lake, but a large percentage of these are undescribed.[36]

History

The Baikal area has a long history of human habitation. An early known tribe in the area was the Kurykans, forefathers of two ethnic groups: the Buryats and Yakuts.

Lake Baikal was situated in the northern territory of the Xiongnu confederation, and was a site of the Han–Xiongnu War, where the armies of the Han dynasty pursued and defeated the Xiongnu forces from the second century BC to the first century AD. They recorded that the lake was a "huge sea" (hanhai) and designated it the North Sea (Běihǎi) of the semimythical Four Seas.[37] The Kurykans, a Siberian tribe who inhabited the area in the sixth century, gave it a name that translates to "much water". Later on, it was called "natural lake" (Baygal nuur) by the Buryats and "rich lake" (Bay göl) by the Yakuts.[38] Little was known to Europeans about the lake until Russia expanded into the area in the 17th century. The first Russian explorer to reach Lake Baikal was Kurbat Ivanov in 1643.[39]

Russian expansion into the Buryat area around Lake Baikal[40] in 1628–1658 was part of the Russian conquest of Siberia. It was done first by following the Angara River upstream from Yeniseysk (founded 1619) and later by moving south from the Lena River. Russians first heard of the Buryats in 1609 at Tomsk. According to folktales related a century after the fact, in 1623, Demid Pyanda, who may have been the first Russian to reach the Lena, crossed from the upper Lena to the Angara and arrived at Yeniseysk.[41] Vikhor Savin (1624) and Maksim Perfilyev (1626 and 1627–1628) explored Tungus country on the lower Angara. To the west, Krasnoyarsk on the upper Yenisei was founded in 1627. There were a number of ill-documented expeditions eastward from Krasnoyarsk. In 1628, Pyotr Beketov first encountered a group of Buryats and collected yasak from them at the future site of Bratsk. In 1629, Yakov Khripunov set off from Tomsk to find a rumored silver mine. His men soon began plundering both Russians and natives. They were joined by another band of rioters from Krasnoyarsk, but left the Buryat country when they ran short of food. This made it difficult for other Russians to enter the area. In 1631, Maksim Perfilyev built an ostrog at Bratsk. The pacification was moderately successful, but in 1634, Bratsk was destroyed and its garrison killed. In 1635, Bratsk was restored by a punitive expedition under Radukovskii. In 1638, it was besieged unsuccessfully.

In 1638, Perfilyev crossed from the Angara over the Ilim portage to the Lena River and went downstream as far as Olyokminsk. Returning, he sailed up the Vitim River into the area east of Lake Baikal (1640) where he heard reports of the Amur country. In 1641, Verkholensk was founded on the upper Lena. In 1643, Kurbat Ivanov went further up the Lena and became the first Russian to see Lake Baikal and Olkhon Island. Half his party under Skorokhodov remained on the lake, reached the Upper Angara at its northern tip and wintered on the Barguzin River on the northeast side. In 1644, Ivan Pokhabov went up the Angara to Baikal, becoming perhaps the first Russian to use this route which is difficult because of the rapids. He crossed the lake and explored the lower Selenge River. About 1647, he repeated the trip, obtained guides and visited a 'Tsetsen Khan' near Ulan Bator. In 1648, Ivan Galkin built an ostrog on the Barguzin River which became a center for eastward expansion. In 1652, Vasily Kolesnikov reported from Barguzin that one could reach the Amur country by following the Selenga, Uda, and Khilok Rivers to the future sites of Chita and Nerchinsk. In 1653, Pyotr Beketov took Kolesnikov's route to Lake Irgen west of Chita, and that winter his man Urasov founded Nerchinsk. Next spring, he tried to occupy Nerchensk, but was forced by his men to join Stephanov on the Amur. Nerchinsk was destroyed by the local Tungus, but restored in 1658.

The Trans-Siberian Railway was built between 1896 and 1902. Construction of the scenic railway around the southwestern end of Lake Baikal required 200 bridges and 33 tunnels. Until its completion, a train ferry transported railcars across the lake from Port Baikal to Mysovaya for a number of years. At times during winter freezes, the lake could be crossed on foot—though at risk of frostbite and deadly hypothermia from the cold wind moving unobstructed across flat expanses of ice. In the winter of 1920, the Great Siberian Ice March occurred, when the retreating White Russian Army crossed frozen Lake Baikal. The wind on the exposed lake was so cold, many people died, freezing in place until spring thaw. Beginning in 1956, the impounding of the Irkutsk Dam on the Angara River raised the level of the lake by 1.4 m (4.6 ft).[42]

As the railway was built, a large hydrogeographical expedition headed by F.K. Drizhenko produced the first detailed contour map of the lake bed.[8]

Research

Baikal fishers fish for 15 commercially exploited species. The omul, found only in Baikal, accounts for most of the catch.[43]

Several organizations are carrying out natural research projects on Lake Baikal. Most of them are governmental or associated with governmental organizations. The Baikal Research Centre is an independent research organization carrying out environmental educational and research projects at Lake Baikal.[44]

In July 2008, Russia sent two small submersibles, Mir-1 and Mir-2, to descend 1,592 m (5,223 ft) to the bottom of Lake Baikal to conduct geological and biological tests on its unique ecosystem. Although originally reported as being successful, they did not set a world record for the deepest freshwater dive, reaching a depth of only 1,580 m (5,180 ft).[45] That record is currently held by Anatoly Sagalevich, at 1,637 m (5,371 ft) (also in Lake Baikal aboard a Pisces submersible in 1990).[45][46] Russian scientist and federal politician, Artur Chilingarov, the leader of the mission, took part in the Mir dives[47] as did Russian leader Vladimir Putin.

Since 1993, neutrino research has been conducted at the Baikal Deep Underwater Neutrino Telescope (BDUNT). The Baikal Neutrino Telescope NT-200 is being deployed in Lake Baikal, 3.6 km (2.2 mi) from shore at a depth of 1.1 km (0.68 mi). It consists of 192 optical modules (OMs).[48]

Economy

The lake, nicknamed "the Pearl of Siberia", drew investors from the tourist industry as energy revenues sparked an economic boom.[49] Viktor Grigorov's Grand Baikal in Irkutsk is one of the investors, who planned to build three hotels, creating 570 jobs. In 2007, the Russian government declared the Baikal region a special economic zone. A popular resort in Listvyanka is home to the seven-story Hotel Mayak. At the northern part of the lake, Baikalplan (a German NGO) built together with Russians in 2009 the Frolikha Adventure Coastline Track, a 100-kilometer (62 mi)-long long-distance trail as example for a sustainable development of the region. Baikal was also declared a UNESCO World Heritage site in 1996. Rosatom plans to build a laboratory in Baikal, in conjunction with an international uranium plant and to invest $2.5 billion in the region and create 2,000 jobs in the city of Angarsk.[49]

Tourism industry on Lake Baikal
A lake surrounded forested hills with a small boat in the distance
Recreational boaters on Chivyrkuisky Bay 
A sandy beach showing cabins and boats drawn up on the shore
Sportfishing boats on Lake Baikal 
A man pulling two sledges on a frozen lake, approaching a crack in the ice
Czech adventure tourist crosses the frozen lake 
Interior of a wooden structure containing a spa pool, with people
A thermal spa at Zagza in the Kabansky District 

Environmental concerns

Baykalsk Pulp and Paper Mill

Baykalsk Pulp and Paper Mill

The Baykalsk Pulp and Paper Mill was constructed in 1966, directly on the shoreline, bleaching paper with chlorine and discharging waste into Baikal. After decades of protest, the plant was closed in November 2008 due to unprofitability.[50][51] In March 2009, the plant owner announced the paper mill would never reopen.[52] However, on 4 January 2010, the production was resumed. On 13 January 2010, Vladimir Putin introduced changes in the legislation legalising the operation of the mill, which brought about a wave of protests of ecologists and local residents.[53] This was based on Putin's visual verification from a minisubmarine, "I could see with my own eyes — and scientists can confirm — Baikal is in good condition and there is practically no pollution".[54] In September 2013, the mill underwent a final bankruptcy, with the last 800 workers slated to lose their jobs by 28 December 2013.[55]

Planned East Siberia-Pacific Ocean oil pipeline

The lake in the winter, as seen from the tourist resort of Listvyanka: The ice is thick enough to support pedestrians and snowmobiles.

Russian oil pipelines state company Transneft[56] was planning to build a trunk pipeline that would have come within 800 meters (2,600 ft) of the lake shore in a zone of substantial seismic activity. Environmental activists in Russia,[57] Greenpeace, Baikal pipeline opposition[58] and local citizens[59] were strongly opposed to these plans, due to the possibility of an accidental oil spill that might cause significant damage to the environment. According to the Transneft's president, numerous meetings with citizens near the lake were held in towns along the route, especially in Irkutsk.[60] However, it was not until Russian president Vladimir Putin ordered the company to consider an alternative route 40 kilometers (25 mi) to the north to avoid such ecological risks that Transneft agreed to alter its plans.[61] Transneft has since decided to move the pipeline away from Lake Baikal, so that it will not pass through any federal or republic natural reserves.[62][63] Work began on the pipeline, two days after President Putin agreed to changing the route away from Lake Baikal.[64]

Proposed nuclear plant

In 2006, the Russian government announced plans to build the world's first International Uranium Enrichment Centre at an existing nuclear facility in Angarsk, 95 km (59 mi) from the lake's shores. However, critics and environmentalists argue it would be a disaster for the region and are urging the government to reconsider.[65]

After enrichment, only 10% of the uranium-derived radioactive material would be exported to international customers,[65] leaving 90% in the Lake Baikal region for storage. Uranium tailings contain radioactive and toxic materials, which if improperly stored, are potentially dangerous to humans and can contaminate rivers and lakes.[65]

Other pollutions sources

According to The Moscow Times, increasing amount invasive species of algae thrive in the lake from hundreds of tons of liquid waste, including fuel and excrement, regularly disposed into the lake by tourist sites; and up to 25,000 tons of liquid waste disposed every year by local ships.[66]

Historical traditions

An 1883 British map using the More Baikal (Baikal Sea) designation, rather than the conventional Ozero Baikal (Lake Baikal)

The first European to reach the lake is said to be Kurbat Ivanov in 1643.[67]

In the past, the Baikal was referred to by many Russians as the "Baikal Sea" (Russian: Море Байкал, More Baikal), rather than merely "Lake Baikal" (Russian: Озеро Байкал, Ozero Baikal).[68] This usage is attested already on the late-17th century maps by Semyon Remezov.[69] To this day, the strait between the western shore of the Lake and the Olkhon Island is called Maloye More (Малое Море), i.e. "the Little Sea".

Lake Baikal is nicknamed "Older sister of Sister Lakes (Lake Khövsgöl and Lake Baikal)".[citation needed]

According to 19th-century traveler T. W. Atkinson, locals in the Lake Baikal Region had the tradition that Christ visited the area:
The people have a tradition in connection with this region which they implicitly believe. They say "that Christ visited this part of Asia and ascended this summit, whence he looked down on all the region around. After blessing the country to the northward, he turned towards the south, and looking across the Baikal, he waved his hand, exclaiming 'Beyond this there is nothing.'" Thus they account for the sterility of Daouria, where it is said "no corn will grow."[70]
Lake Baikal has been celebrated in several Russian folk songs. Two of these songs are well known in Russia and its neighboring countries, such as Japan.
  • "The Glorious Sea – Sacred Baikal" (in Russian: Славное Mope, Священный Байкал) is about a katorga fugitive. The lyrics as documented and edited in the 19th century by Dmitriy P. Davydov (1811–1888).[71] See "Barguzin River" for sample lyrics.
The latter song was a secondary theme song for the Soviet Union's second color film, Ballad of Siberia (1947; in Russian: Сказание о земле Сибирской).

In popular culture

  • In The Way Back (2010) and the memoir on which it is based, The Long Walk (1955), Lake Baikal is a major landmark and waystation for a group of men who escaped from a Siberian Gulag, and the point where the group meets up with Irena, a Polish orphan

Gallery

African Great Lakes

African Great Lakes

From Wikipedia, the free encyclopedia

Satellite view of the African Great Lakes region and its coastline.

The African Great Lakes (Swahili: Maziwa Makuu) are a series of lakes constituting the part of the Rift Valley lakes in and around the East African Rift. They include Lake Victoria, the second largest fresh water lake in the world, and Lake Tanganyika, the world's second largest in volume as well as the second deepest.[1] The term Greater Lakes is also used, less commonly, for some of them. Countries in the African Great Lakes region include Burundi, the Democratic Republic of Congo, Kenya, Rwanda, Tanzania and Uganda.[2]

Catchments

A – Albert
Y – Kyoga
E – Edward
K – Kivu
V – Victoria
T – Tanganyika
M – Malawi

The African Great Lakes are divided among three different catchments (river basins); a number, such as Lake Turkana, also have internal drainage systems. The following, in order of size from largest to smallest, are included on most lists of the African Great Lakes:
Some call only Lake Victoria, Lake Albert, and Lake Edward the Great Lakes, as they are the only three that empty into the White Nile. Lake Kyoga is part of the Great Lakes system. However, it is not itself considered a Great Lake, based on size alone. Lake Tanganyika and Lake Kivu both empty into the Congo River system, while Lake Malawi is drained by the Shire River into the Zambezi. Lake Turkana has no outlet.

African Great Lakes region

The African Great Lake region consists of countries that surround the African Great Lakes. It comprises Burundi, the Democratic Republic of Congo, Kenya, Rwanda, Tanzania and Uganda.[2]
The Bantu Swahili language is the most commonly spoken language in the African Great Lakes region.[3] It also serves as a national or official language of four nations in the region: Tanzania, Kenya, Uganda and the Democratic Republic of the Congo.

Due to the density of population and the agricultural surplus in the region, the area became organized into a number of small states. The most powerful of these monarchies were Rwanda, Burundi, Buganda, and Bunyoro. Unusual for sub-Saharan Africa, the traditional borders were largely maintained by the colonial powers.

Being the long sought after source of the Nile, the region had long been of interest to Europeans. The first Europeans to arrive in the region in any numbers were missionaries who had limited success in converting the locals, but did open the region to later colonization. The increased contact with the rest of the world led to a series of devastating epidemics affecting both humans and livestock. While seen as a region with great potential after independence, the region has in recent decades been marred by civil war and conflict, from which only Tanzania has largely escaped. The worst affected areas have been left in great poverty.

Education

From Wikipedia, the free encyclopedia https://en.wikipedia.org/wiki/Education Education is the transmissio...