Misplaced Pages

#183816

148-475: The sanctuary was first notified in 1981 covering an area of 765.79 square kilometres (295.67 sq mi). In 1992, the Gujarat state government's department of mining and geology pointed out that there were huge deposits of limestone , lignite (brown coal), bentonite and bauxite inside the protected area of the sanctuary and argued that the ban on mining in the sanctuary was holding back development of

296-455: A Mohs hardness of 2 to 4, dense limestone can have a crushing strength of up to 180 MPa . For comparison, concrete typically has a crushing strength of about 40 MPa. Although limestones show little variability in mineral composition, they show great diversity in texture. However, most limestone consists of sand-sized grains in a carbonate mud matrix. Because limestones are often of biological origin and are usually composed of sediment that

444-463: A bloom of cyanobacteria or microalgae . However, stable isotope ratios in modern carbonate mud appear to be inconsistent with either of these mechanisms, and abrasion of carbonate grains in high-energy environments has been put forward as a third possibility. Formation of limestone has likely been dominated by biological processes throughout the Phanerozoic , the last 540 million years of

592-555: A basis for the development of a bio-inspired method of desalination . Uptake of Na ions is desirable for halophytes to build up osmotic potential , absorb water and sustain turgor pressure . However, excess Na ions may work on toxic element. Therefore, halophytes try to adjust salinity delicately between growth and survival strategies. In this point of view, a novel sustainable desalination method can be derived from halophytes, which are in contact with saline water through their roots. Halophytes exclude salt through their roots, secrete

740-434: A carbonate rock outcrop can be estimated in the field by etching the surface with dilute hydrochloric acid. This etches away the calcite and aragonite, leaving behind any silica or dolomite grains. The latter can be identified by their rhombohedral shape. Crystals of calcite, quartz , dolomite or barite may line small cavities ( vugs ) in the rock. Vugs are a form of secondary porosity, formed in existing limestone by

888-616: A central quartz grain or carbonate mineral fragment. These likely form by direct precipitation of calcium carbonate onto the ooid. Pisoliths are similar to ooids, but they are larger than 2 mm in diameter and tend to be more irregular in shape. Limestone composed mostly of ooids is called an oolite or sometimes an oolitic limestone . Ooids form in high-energy environments, such as the Bahama platform, and oolites typically show crossbedding and other features associated with deposition in strong currents. Oncoliths resemble ooids but show

1036-449: A change in environment that increases the solubility of calcite. Dense, massive limestone is sometimes described as "marble". For example, the famous Portoro "marble" of Italy is actually a dense black limestone. True marble is produced by recrystallization of limestone during regional metamorphism that accompanies the mountain building process ( orogeny ). It is distinguished from dense limestone by its coarse crystalline texture and

1184-589: A complex salt filtration system and a complex root system to cope with saltwater immersion and wave action. They are adapted to the low-oxygen conditions of waterlogged mud, but are most likely to thrive in the upper half of the intertidal zone . The mangrove biome , often called the mangrove forest or mangal, is a distinct saline woodland or shrubland habitat characterized by depositional coastal environments, where fine sediments (often with high organic content) collect in areas protected from high-energy wave action. Mangrove forests serve as vital habitats for

1332-949: A composition reflecting the organisms that produced them and the environment in which they were produced. Low-magnesium calcite skeletal grains are typical of articulate brachiopods , planktonic (free-floating) foraminifera, and coccoliths . High-magnesium calcite skeletal grains are typical of benthic (bottom-dwelling) foraminifera, echinoderms , and coralline algae . Aragonite skeletal grains are typical of molluscs , calcareous green algae , stromatoporoids , corals , and tube worms . The skeletal grains also reflect specific geological periods and environments. For example, coral grains are more common in high-energy environments (characterized by strong currents and turbulence) while bryozoan grains are more common in low-energy environments (characterized by quiet water). Ooids (sometimes called ooliths) are sand-sized grains (less than 2mm in diameter) consisting of one or more layers of calcite or aragonite around

1480-412: A considerable fraction of the limestone bed. At depths greater than 1 km (0.62 miles), burial cementation completes the lithification process. Burial cementation does not produce stylolites. When overlying beds are eroded, bringing limestone closer to the surface, the final stage of diagenesis takes place. This produces secondary porosity as some of the cement is dissolved by rainwater infiltrating

1628-468: A critical food source for larger predators like birds, reptiles, and mammals within the ecosystem. Additionally, mangrove forests function as essential nurseries for many commercially important fish species, providing a sheltered environment rich in nutrients during their early life stages. The decomposition of leaves and organic matter in the water further enhances the nutrient content, supporting overall ecosystem productivity. In summary, mangrove forests play

SECTION 10

#1732776696184

1776-434: A crucial and unbiased role in sustaining biodiversity and ecological balance within coastal food webs. Larger marine organisms benefit from the habitat as a nursery for their offspring. Lemon sharks depend on mangrove creeks to give birth to their pups. The ecosystem provides little competition and minimizes threats of predation to juvenile lemon sharks as they use the cover of mangroves to practice hunting before entering

1924-534: A diverse array of aquatic species, offering a unique ecosystem that supports the intricate interplay of marine life and terrestrial vegetation. The saline conditions tolerated by various mangrove species range from brackish water, through pure seawater (3 to 4% salinity), to water concentrated by evaporation to over twice the salinity of ocean seawater (up to 9% salinity). Beginning in 2010, remote sensing technologies and global data have been used to assess areas, conditions and deforestation rates of mangroves around

2072-483: A drop of dilute hydrochloric acid is dropped on it. Dolomite is also soft but reacts only feebly with dilute hydrochloric acid, and it usually weathers to a characteristic dull yellow-brown color due to the presence of ferrous iron. This is released and oxidized as the dolomite weathers. Impurities (such as clay , sand, organic remains, iron oxide , and other materials) will cause limestones to exhibit different colors, especially with weathered surfaces. The makeup of

2220-637: A few million years, as this is the most stable form of calcium carbonate. Ancient carbonate formations of the Precambrian and Paleozoic contain abundant dolomite, but limestone dominates the carbonate beds of the Mesozoic and Cenozoic . Modern dolomite is quite rare. There is evidence that, while the modern ocean favors precipitation of aragonite, the oceans of the Paleozoic and middle to late Cenozoic favored precipitation of calcite. This may indicate

2368-455: A few thousand years. As rainwater mixes with groundwater, aragonite and high-magnesium calcite are converted to low-calcium calcite. Cementing of thick carbonate deposits by rainwater may commence even before the retreat of the sea, as rainwater can infiltrate over 100 km (60 miles) into sediments beneath the continental shelf. As carbonate sediments are increasingly deeply buried under younger sediments, chemical and mechanical compaction of

2516-452: A fundamental environmental index for future reference. Mangrove forests are one of the most carbon-rich biomes, accounting for 11% of the total input of terrestrial carbon into oceans. Viruses are thought to significantly influence local and global biogeochemical cycles , though as of 2019 little information was available about the community structure, genetic diversity and ecological roles of viruses in mangrove ecosystems. Viruses are

2664-470: A given mangrove swamp typically features only a small number of tree species. It is not uncommon for a mangrove forest in the Caribbean to feature only three or four tree species. For comparison, the tropical rainforest biome contains thousands of tree species, but this is not to say mangrove forests lack diversity. Though the trees themselves are few in species, the ecosystem that these trees create provides

2812-622: A global annual deforestation rate estimated at 0.16%, and per-country rates as high as 0.70%. Degradation in quality of remaining mangroves is also an important concern. There is interest in mangrove restoration for several reasons. Mangroves support sustainable coastal and marine ecosystems. They protect nearby areas from tsunamis and extreme weather events. Mangrove forests are also effective at carbon sequestration and storage. The success of mangrove restoration may depend heavily on engagement with local stakeholders, and on careful assessment to ensure that growing conditions will be suitable for

2960-464: A hierarchical, triple layered pore structure in the epidermis and most Na ions are filtered at the first sublayer of the outermost layer. The high blockage of Na ions is attributed to the high surface zeta potential of the first layer. The second layer, which is composed of macroporous structures , also facilitates Na ion filtration. The study provides insights into the mechanism underlying water filtration through halophyte roots and could serve as

3108-411: A higher concentration of white mangroves. Mangrove forests are an important part of the cycling and storage of carbon in tropical coastal ecosystems. Knowing this, scientists seek to reconstruct the environment and investigate changes to the coastal ecosystem over thousands of years using sediment cores. However, an additional complication is the imported marine organic matter that also gets deposited in

SECTION 20

#1732776696184

3256-480: A home (habitat) for a great variety of other species, including as many as 174 species of marine megafauna . Mangrove plants require a number of physiological adaptations to overcome the problems of low environmental oxygen levels, high salinity , and frequent tidal flooding . Each species has its own solutions to these problems; this may be the primary reason why, on some shorelines, mangrove tree species show distinct zonation. Small environmental variations within

3404-410: A key role in maintaining prey species along coastlines and within mangrove ecosystems. Mangrove forests can decay into peat deposits because of fungal and bacterial processes as well as by the action of termites . It becomes peat in good geochemical , sedimentary, and tectonic conditions. The nature of these deposits depends on the environment and the types of mangroves involved. In Puerto Rico ,

3552-700: A large number of bird species (terrestrial and aquatic) including 19 identified species of raptors . The avifauna study of the sanctuary was specifically undertaken at the initiative of the Gujarat Institute of Desert Ecology, in 1997–98 to evolve a 'Management Plan' that conserves the bird species. The study has identified 161 species (46 families) of which 112 are resident species (of 36 families) and 38 are migrants – majority are wetland birds – belonging to 13 families, vis-a-vis an earlier study that had identified 112 species of 36 families of which 23 were migrants. The study also provides detailed information of

3700-435: A limestone sample except in thin section and are less common in ancient limestones, possibly because compaction of carbonate sediments disrupts them. Limeclasts are fragments of existing limestone or partially lithified carbonate sediments. Intraclasts are limeclasts that originate close to where they are deposited in limestone, while extraclasts come from outside the depositional area. Intraclasts include grapestone , which

3848-407: A long history to survive against harsh environmental conditions. In this harsh environment, mangroves have evolved a special mechanism to help their offspring survive. Mangrove seeds are buoyant and are therefore suited to water dispersal. Unlike most plants, whose seeds germinate in soil, many mangroves (e.g. red mangrove ) are viviparous , meaning their seeds germinate while still attached to

3996-471: A lower Mg/Ca ratio in the ocean water of those times. This magnesium depletion may be a consequence of more rapid sea floor spreading , which removes magnesium from ocean water. The modern ocean and the ocean of the Mesozoic have been described as "aragonite seas". Most limestone was formed in shallow marine environments, such as continental shelves or platforms . Such environments form only about 5% of

4144-525: A lower diversity of organisms and a greater fraction of silica and clay minerals characteristic of marls . The Green River Formation is an example of a prominent freshwater sedimentary formation containing numerous limestone beds. Freshwater limestone is typically micritic. Fossils of charophyte (stonewort), a form of freshwater green algae, are characteristic of these environments, where the charophytes produce and trap carbonates. Limestones may also form in evaporite depositional environments . Calcite

4292-457: A mangal may lead to greatly differing methods for coping with the environment. Therefore, the mix of species is partly determined by the tolerances of individual species to physical conditions, such as tidal flooding and salinity, but may also be influenced by other factors, such as crabs preying on plant seedlings. Once established, mangrove roots provide an oyster habitat and slow water flow, thereby enhancing sediment deposition in areas where it

4440-523: A mechanism for dolomitization, with one 2004 review paper describing it bluntly as "a myth". Ordinary seawater is capable of converting calcite to dolomite, if the seawater is regularly flushed through the rock, as by the ebb and flow of tides (tidal pumping). Once dolomitization begins, it proceeds rapidly, so that there is very little carbonate rock containing mixed calcite and dolomite. Carbonate rock tends to be either almost all calcite/aragonite or almost all dolomite. About 20% to 25% of sedimentary rock

4588-448: A plausible source of mud. Another possibility is direct precipitation from the water. A phenomenon known as whitings occurs in shallow waters, in which white streaks containing dispersed micrite appear on the surface of the water. It is uncertain whether this is freshly precipitated aragonite or simply material stirred up from the bottom, but there is some evidence that whitings are caused by biological precipitation of aragonite as part of

Narayan Sarovar Sanctuary - Misplaced Pages Continue

4736-451: A quiet marine habitat for young organisms. In areas where roots are permanently submerged, the organisms they host include algae , barnacles , oysters , sponges , and bryozoans , which all require a hard surface for anchoring while they filter-feed. Shrimps and mud lobsters use the muddy bottoms as their home. Mangrove crabs eat the mangrove leaves, adding nutrients to the mangal mud for other bottom feeders. In at least some cases,

4884-449: A radial rather than layered internal structure, indicating that they were formed by algae in a normal marine environment. Peloids are structureless grains of microcrystalline carbonate likely produced by a variety of processes. Many are thought to be fecal pellets produced by marine organisms. Others may be produced by endolithic (boring) algae or other microorganisms or through breakdown of mollusc shells. They are difficult to see in

5032-455: A recent analysis of Pacific Ocean Virome data identified niche-specialised AMGs that contribute to depth-stratified host adaptations. Given that microbes drive global biogeochemical cycles, and a large fraction of microbes is infected by viruses at any given time, viral-encoded AMGs must play important roles in global biogeochemistry and microbial metabolic evolution. Mangrove forests are the only woody halophytes that live in salt water along

5180-570: A repertoire of microbial taxa that contribute to important ecological functions in mangrove ecosystems. Like typical terrestrial plants, mangroves depend upon mutually beneficial interactions with microbial communities. In particular, microbes residing in developed roots could help mangroves transform nutrients into usable forms before plant assimilation. These microbes also provide mangroves phytohormones for suppressing phytopathogens or helping mangroves withstand heat and salinity. In turn, root-associated microbes receive carbon metabolites from

5328-402: A week, simulating frequent tropical rainstorms. A 2016 study by Kim et al. investigated the biophysical characteristics of sea water filtration in the roots of the mangrove Rhizophora stylosa from a plant hydrodynamic point of view. R. stylosa can grow even in saline water and the salt level in its roots is regulated within a certain threshold value through filtration. The root possesses

5476-405: A year before arriving in a suitable environment. Once a propagule is ready to root, its density changes so that the elongated shape now floats vertically rather than horizontally. In this position, it is more likely to lodge in the mud and root. If it does not root, it can alter its density and drift again in search of more favorable conditions. The following listings, based on Tomlinson, 2016, give

5624-495: Is 2.7 metres (8.9 ft) ( above mean sea level ). In the hill section it is 157 metres (515 ft) (a.m.s.l) at Manijal hill in Kaniyaro Rakhal. The rivers and streams flowing through the sanctuary are small and ephemeral in nature (Kapurasi and Kali are the two river systems) since rainfall is very scanty and erratic. Surface water is being harnessed at 15 reservoirs that surround the sanctuary. Ground water potential

5772-497: Is a shrub or tree that grows mainly in coastal saline or brackish water . Mangroves grow in an equatorial climate, typically along coastlines and tidal rivers. They have particular adaptations to take in extra oxygen and remove salt, allowing them to tolerate conditions that kill most plants. The term is also used for tropical coastal vegetation consisting of such species. Mangroves are taxonomically diverse due to convergent evolution in several plant families. They occur worldwide in

5920-705: Is already occurring. The fine, anoxic sediments under mangroves act as sinks for a variety of heavy (trace) metals which colloidal particles in the sediments have concentrated from the water. Mangrove removal disturbs these underlying sediments, often creating problems of trace metal contamination of seawater and organisms of the area. Mangrove swamps protect coastal areas from erosion , storm surge (especially during tropical cyclones ), and tsunamis . They limit high-energy wave erosion mainly during events such as storm surges and tsunamis. The mangroves' massive root systems are efficient at dissipating wave energy. Likewise, they slow down tidal water so that its sediment

6068-560: Is also favored on the seaward margin of shelves and platforms, where there is upwelling deep ocean water rich in nutrients that increase organic productivity. Reefs are common here, but when lacking, ooid shoals are found instead. Finer sediments are deposited close to shore. The lack of deep sea limestones is due in part to rapid subduction of oceanic crust, but is more a result of dissolution of calcium carbonate at depth. The solubility of calcium carbonate increases with pressure and even more with higher concentrations of carbon dioxide, which

Narayan Sarovar Sanctuary - Misplaced Pages Continue

6216-401: Is also mentioned, as their numbers are reported to be small. there is one more species of rabbit is can be seen because of animal friendly peoples and good environmental conditions and fox also here in good condition and national bird is here and easily visible and no. of reptiles are present here some are poisonous and some are friendly An interpretation centre at Loriya next to the sanctuary

6364-399: Is an obsolete and poorly-defined term used variously for dolomite, for limestone containing significant dolomite ( dolomitic limestone ), or for any other limestone containing a significant percentage of magnesium . Most limestone was formed in shallow marine environments, such as continental shelves or platforms , though smaller amounts were formed in many other environments. Much dolomite

6512-482: Is an uncommon mineral in limestone, and siderite or other carbonate minerals are rare. However, the calcite in limestone often contains a few percent of magnesium . Calcite in limestone is divided into low-magnesium and high-magnesium calcite, with the dividing line placed at a composition of 4% magnesium. High-magnesium calcite retains the calcite mineral structure, which is distinct from dolomite. Aragonite does not usually contain significant magnesium. Most limestone

6660-402: Is carbonate rock, and most of this is limestone. Limestone is found in sedimentary sequences as old as 2.7 billion years. However, the compositions of carbonate rocks show an uneven distribution in time in the geologic record. About 95% of modern carbonates are composed of high-magnesium calcite and aragonite. The aragonite needles in carbonate mud are converted to low-magnesium calcite within

6808-474: Is clusters of peloids cemented together by organic material or mineral cement. Extraclasts are uncommon, are usually accompanied by other clastic sediments, and indicate deposition in a tectonically active area or as part of a turbidity current . The grains of most limestones are embedded in a matrix of carbonate mud. This is typically the largest fraction of an ancient carbonate rock. Mud consisting of individual crystals less than 5 μm (0.20 mils) in length

6956-416: Is commonly white to gray in color. Limestone that is unusually rich in organic matter can be almost black in color, while traces of iron or manganese can give limestone an off-white to yellow to red color. The density of limestone depends on its porosity, which varies from 0.1% for the densest limestone to 40% for chalk. The density correspondingly ranges from 1.5 to 2.7 g/cm . Although relatively soft, with

7104-406: Is composed mostly of the minerals calcite and aragonite , which are different crystal forms of CaCO 3 . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for

7252-420: Is controlled largely by the amount of dissolved carbon dioxide ( CO 2 ) in the water. This is summarized in the reaction: Increases in temperature or decreases in pressure tend to reduce the amount of dissolved CO 2 and precipitate CaCO 3 . Reduction in salinity also reduces the solubility of CaCO 3 , by several orders of magnitude for fresh water versus seawater. Near-surface water of

7400-545: Is converted to low-magnesium calcite. Diagenesis is the likely origin of pisoliths , concentrically layered particles ranging from 1 to 10 mm (0.039 to 0.394 inches) in diameter found in some limestones. Pisoliths superficially resemble ooids but have no nucleus of foreign matter, fit together tightly, and show other signs that they formed after the original deposition of the sediments. Silicification occurs early in diagenesis, at low pH and temperature, and contributes to fossil preservation. Silicification takes place through

7548-416: Is deposited as the tide comes in, leaving all except fine particles when the tide ebbs. In this way, mangroves build their environments. Because of the uniqueness of mangrove ecosystems and the protection against erosion they provide, they are often the object of conservation programs, including national biodiversity action plans . The unique ecosystem found in the intricate mesh of mangrove roots offers

SECTION 50

#1732776696184

7696-503: Is deposited close to where it formed, classification of limestone is usually based on its grain type and mud content. Most grains in limestone are skeletal fragments of marine organisms such as coral or foraminifera . These organisms secrete structures made of aragonite or calcite, and leave these structures behind when they die. Other carbonate grains composing limestones are ooids , peloids , and limeclasts ( intraclasts and extraclasts  [ ca ] ). Skeletal grains have

7844-460: Is described as coquinite . Chalk is a soft, earthy, fine-textured limestone composed of the tests of planktonic microorganisms such as foraminifera, while marl is an earthy mixture of carbonates and silicate sediments. Limestone forms when calcite or aragonite precipitate out of water containing dissolved calcium, which can take place through both biological and nonbiological processes. The solubility of calcium carbonate ( CaCO 3 )

7992-617: Is described as micrite . In fresh carbonate mud, micrite is mostly small aragonite needles, which may precipitate directly from seawater, be secreted by algae, or be produced by abrasion of carbonate grains in a high-energy environment. This is converted to calcite within a few million years of deposition. Further recrystallization of micrite produces microspar , with grains from 5 to 15 μm (0.20 to 0.59 mils) in diameter. Limestone often contains larger crystals of calcite, ranging in size from 0.02 to 0.1 mm (0.79 to 3.94 mils), that are described as sparry calcite or sparite . Sparite

8140-462: Is distinguished from micrite by a grain size of over 20 μm (0.79 mils) and because sparite stands out under a hand lens or in thin section as white or transparent crystals. Sparite is distinguished from carbonate grains by its lack of internal structure and its characteristic crystal shapes. Geologists are careful to distinguish between sparite deposited as cement and sparite formed by recrystallization of micrite or carbonate grains. Sparite cement

8288-422: Is good in view of black loamy soil found here, which is fertile and has better moisture retaining capacity. The sanctuary has a tropical climate where summer is very hot. The arid climate has recorded maximum temperature varying from 40–42 °C (104–108 °F) and a minimum of 10–12 °C (50–54 °F). During summer, May and June are the hottest months with dusty storms. In winter, December and January are

8436-403: Is known to be harmful to the environment resulting in the release of large clouds of dust. Environmentalists feared that in the arid region of Kachchh district, these dust clouds would have harmful effects on both vegetation and wildlife as the limestone dust would condense in the cool nights settling on the leaves proving disastrous for the forests in the vicinity. Several environment groups in

8584-427: Is meagre and water is saline in the sanctuary area. The number of villages in the sanctuary at present is reported to be 32 (1997–98) vis-à-vis 56 villages before de-notification of 1995. It is also reported that the sanctuary has been subjected to deforestation due to anthropogenic pressures; with the mining activities permitted after de-notification causing considerable stress on the sanctuary. Geological formations in

8732-560: Is one of the first minerals to precipitate in marine evaporites. Most limestone is formed by the activities of living organisms near reefs, but the organisms responsible for reef formation have changed over geologic time. For example, stromatolites are mound-shaped structures in ancient limestones, interpreted as colonies of cyanobacteria that accumulated carbonate sediments, but stromatolites are rare in younger limestones. Organisms precipitate limestone both directly as part of their skeletons, and indirectly by removing carbon dioxide from

8880-473: Is otherwise chemically fairly pure, with clastic sediments (mainly fine-grained quartz and clay minerals ) making up less than 5% to 10% of the composition. Organic matter typically makes up around 0.2% of a limestone and rarely exceeds 1%. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragments (such as sponge spicules, diatoms , or radiolarians ). Fossils are also common in limestone. Limestone

9028-472: Is produced by decaying organic matter settling into the deep ocean that is not removed by photosynthesis in the dark depths. As a result, there is a fairly sharp transition from water saturated with calcium carbonate to water unsaturated with calcium carbonate, the lysocline , which occurs at the calcite compensation depth of 4,000 to 7,000 m (13,000 to 23,000 feet). Below this depth, foraminifera tests and other skeletal particles rapidly dissolve, and

SECTION 60

#1732776696184

9176-461: Is reported to be higher than in well-preserved mangroves Studies comparing mangroves in different conservation states show that bacterial composition in disturbed mangrove sediment alters its structure, leading to a functional equilibrium, where the dynamics of chemicals in mangrove soils lead to the remodeling of its microbial structure. Despite many research advancements in mangrove sediment bacterial metagenomics diversity in various conditions over

9324-518: Is secondary dolomite, formed by chemical alteration of limestone. Limestone is exposed over large regions of the Earth's surface, and because limestone is slightly soluble in rainwater, these exposures often are eroded to become karst landscapes. Most cave systems are found in limestone bedrock. Limestone has numerous uses: as a chemical feedstock for the production of lime used for cement (an essential component of concrete ), as aggregate for

9472-492: Is stored in soil and sizable belowground pools of dead roots, aiding in the conservation and recycling of nutrients beneath forests. Although mangroves cover only 0.5% of the earth's coastal area, they account for 10–15% of the coastal sediment carbon storage and 10–11% of the total input of terrestrial carbon into oceans. The disproportionate contribution of mangroves to carbon sequestration is now perceived as an important means to counterbalance greenhouse gas emissions. Despite

9620-579: Is stored in the sediment and the carbon cycle continues. Mangroves are an important source of blue carbon . Globally, mangroves stored 4.19 Gt (9.2 × 10  lb) of carbon in 2012. Two percent of global mangrove carbon was lost between 2000 and 2012, equivalent to a maximum potential of 0.316996250 Gt (6.9885710 × 10  lb) of emissions of carbon dioxide in Earth's atmosphere . Globally, mangroves have been shown to provide measurable economic protections to coastal communities affected by tropical storms. Plant microbiomes play crucial roles in

9768-462: Is the main species which covers an extensive area in the eastern zone while babul is the dominant species in the western zone where limestone is the geological formation in some of the patches. The invasive species Prosopis juliflora is noted to be spreading in the sanctuary resulting in decrease of grassy and herbaceous patches. The invasive vegetation of Prosopis chilensis is reported in an area of 12.39 square kilometres (4.78 sq mi) in

9916-568: The Malay language manggi-manggi The English usage may reflect a corruption via folk etymology of the words mangrow and grove . The word "mangrove" is used in at least three senses: According to Hogarth (2015), among the recognized mangrove species there are about 70 species in 20 genera from 16 families that constitute the "true mangroves" – species that occur almost exclusively in mangrove habitats. Demonstrating convergent evolution , many of these species found similar solutions to

10064-480: The bulk soil outside the rhizosphere . Furthermore, it was noted that the root episphere, rather than the rhizosphere, was primarily responsible for controlling the entry of specific microbial populations into the root, resulting in the selective enrichment of Proteobacteria in the endosphere. These findings provide new insights into the niche differentiation of root-associated microbial communities, Nevertheless, amplicon-based community profiling may not provide

10212-570: The central desert of Iran . Thus cheetah experts from around the world have advised India to import and introduce the cheetah from Africa as genetically it is identical to the ones found in Asia, as latest genetic studies have revealed that the Asian population had separated from the African relatively recently only 5000 years ago which is not enough for a subspecies level differentiation. However,

10360-652: The peafowl . The caracal is considered endangered in Gujarat and vulnerable internationally, has been seen now in this sanctuary at Kutch after a lapse of almost 10 years. Gujarat Institute of Desert Ecology (Bhuj) sighted two individuals in February and March 1998. Other species present include honey badger ( Mellivora capensis ), pangolin ( Manis crassicaudata ) and desert fox ( Vulpes vulpes pusila ). Narayan Sarovar Sanctuary and Banni Grasslands , both in Kutch , have been classified by Wildlife Institute of India (WII) as

10508-420: The red , white , and black mangroves occupy different ecological niches and have slightly different chemical compositions, so the carbon content varies between the species, as well between the different tissues of the plant (e.g., leaf matter versus roots). In Puerto Rico, there is a clear succession of these three trees from the lower elevations, which are dominated by red mangroves, to farther inland with

10656-640: The tropics and subtropics and even some temperate coastal areas, mainly between latitudes 30° N and 30° S, with the greatest mangrove area within 5° of the equator . Mangrove plant families first appeared during the Late Cretaceous to Paleocene epochs and became widely distributed in part due to the movement of tectonic plates . The oldest known fossils of mangrove palm date to 75 million years ago. Mangroves are salt-tolerant trees, shrubs and ferns also called halophytes , and are adapted to live in harsh coastal conditions. They contain

10804-678: The 'specialists' were ortolan bunting , desert warbler , pied tit , white-browed fantail , lesser spotted eagle , sirkeer malkoha , Eurasian wryneck and yellow-crowned woodpecker . The faunal diversity consists of 14 species of mammals, nine species of reptiles and six species of snakes. Some of the important ones supported by the sanctuary include: chinkara , blackbuck , caracal , desert cat , pangolin , great Indian bustard, porcupine , blue bull or nilgai ( Boselaphus tragocamelus ), Indian boar ( Sus scrofa ), Indian wolf ( Canis lupus pallipes ), Indian grey mongoose ( Urva edwardsii ), hare , striped hyena ( Hyaena hyaena ) and

10952-496: The Earth's history. Limestone may have been deposited by microorganisms in the Precambrian , prior to 540 million years ago, but inorganic processes were probably more important and likely took place in an ocean more highly oversaturated in calcium carbonate than the modern ocean. Diagenesis is the process in which sediments are compacted and turned into solid rock . During diagenesis of carbonate sediments, significant chemical and textural changes take place. For example, aragonite

11100-538: The North Island but become low scrub toward their southern limit. In both instances, the species is referred to as Avicennia marina var. australis , although genetic comparison is clearly needed. In Western Australia, A. marina extends as far south as Bunbury (33° 19'S). In the northern hemisphere, scrubby Avicennia gerrninans in Florida occurs as far north as St. Augustine on the east coast and Cedar Point on

11248-551: The accumulated salt through their aerial parts and sequester salt in senescent leaves and/or the bark. Mangroves are facultative halophytes and Bruguiera is known for its special ultrafiltration system that can filter approximately 90% of Na ions from the surrounding seawater through the roots. The species also exhibits a high rate of salt rejection. The water-filtering process in mangrove roots has received considerable attention for several decades. Morphological structures of plants and their functions have been evolved through

11396-452: The area. The sanctuary is delimited by the Kori creek on the northwest and mangrove forest on the west, while prominent land features form its northern and southern limits. While the northwest and western part exhibit a flat topography towards the sea shore, the northeastern part has undulating topography of minor hill ranges; the elevation of the sanctuary near the coast (near Tahera village)

11544-490: The avifauna in respect of each habitat of the sanctuary for resident and migratory birds, region wise, season wise and feeding habit wise. The abundant species identified were: grey francolin , Eurasian collared dove , laughing dove , Indian robin , red-vented bulbul , common babbler , house sparrow and plain munia . Greater short-toed lark ( Calandrella brachydactyla ) was the common migratory bird seen here in large numbers. The birds sighted less frequently, called

11692-434: The base of roads, as white pigment or filler in products such as toothpaste or paint, as a soil conditioner , and as a popular decorative addition to rock gardens . Limestone formations contain about 30% of the world's petroleum reservoirs . Limestone is composed mostly of the minerals calcite and aragonite , which are different crystal forms of calcium carbonate ( CaCO 3 ). Dolomite , CaMg(CO 3 ) 2 ,

11840-657: The beds. This may include the formation of vugs , which are crystal-lined cavities within the limestone. Diagenesis may include conversion of limestone to dolomite by magnesium-rich fluids. There is considerable evidence of replacement of limestone by dolomite, including sharp replacement boundaries that cut across bedding. The process of dolomitization remains an area of active research, but possible mechanisms include exposure to concentrated brines in hot environments ( evaporative reflux ) or exposure to diluted seawater in delta or estuary environments ( Dorag dolomitization ). However, Dorag dolomitization has fallen into disfavor as

11988-464: The bottom with the concave face downwards. This traps a void space that can later be filled by sparite. Geologists use geopetal structures to determine which direction was up at the time of deposition, which is not always obvious with highly deformed limestone formations. The cyanobacterium Hyella balani can bore through limestone; as can the green alga Eugamantia sacculata and the fungus Ostracolaba implexa . Mangrove A mangrove

12136-474: The centre would function once funds are allocated. The sanctuary is located 200 kilometres (120 mi) from Bhuj, which is the district headquarters of the Kachchh. Kutch is well connected by road, rail and air links with the rest of the country. Limestone Limestone ( calcium carbonate CaCO 3 ) is a type of carbonate sedimentary rock which is the main source of the material lime . It

12284-445: The coldest months. Rainfall is very meagre; the average annual rainfall of Lakhpat (Dayapar station) is reported as 349.2 millimetres (13.75 in) (average of 25 years data). Evapo-transpiration rate varies between 1,850–1,900 millimetres (73–75 in)/year. The sanctuary harbours not only three types of great Indian bustards and the lesser florican but is also habitat for the black partridge , several species of herpetofauna ,

12432-580: The country challenged the de-notification decision in the courts, claiming it to be illegal because it had not been approved by the Gujarat state legislative assembly. The de-notification was challenged in the High Court of Gujarat and the Supreme Court of India resulting in a legal battle between the Government of Gujarat and the 'Environmental Activists' along with inputs (adverse impacts on

12580-452: The de-notification, the Gujarat state government planned to grant a lease to a cement company for open-cast mining in 2,000 hectares of land inside the original erstwhile Sanctuary to allow the mining of limestone, lignite and bauxite and for other industrial additives as it seemed an ideal location for a cement factory. The country's, or even Asia's, largest cement manufacturing unit was planned to be built there. Open-cast limestone mining

12728-466: The depositional fabric of carbonate rocks. Dunham divides the rocks into four main groups based on relative proportions of coarser clastic particles, based on criteria such as whether the grains were originally in mutual contact, and therefore self-supporting, or whether the rock is characterized by the presence of frame builders and algal mats. Unlike the Folk scheme, Dunham deals with the original porosity of

12876-469: The deposits are highly porous, so that they have a spongelike texture, they are typically described as tufa . Secondary calcite deposited by supersaturated meteoric waters ( groundwater ) in caves is also sometimes described as travertine. This produces speleothems , such as stalagmites and stalactites . Coquina is a poorly consolidated limestone composed of abraded pieces of coral , shells , or other fossil debris. When better consolidated, it

13024-406: The earth's oceans are oversaturated with CaCO 3 by a factor of more than six. The failure of CaCO 3 to rapidly precipitate out of these waters is likely due to interference by dissolved magnesium ions with nucleation of calcite crystals, the necessary first step in precipitation. Precipitation of aragonite may be suppressed by the presence of naturally occurring organic phosphates in

13172-509: The ecological importance of mangrove ecosystem, knowledge on mangrove biodiversity is notably limited. Previous reports mainly investigated the biodiversity of mangrove fauna, flora and bacterial communities. Particularly, little information is available about viral communities and their roles in mangrove soil ecosystems. In view of the importance of viruses in structuring and regulating host communities and mediating element biogeochemical cycles, exploring viral communities in mangrove ecosystems

13320-448: The edaphic climax of the forest, the tree height in the sanctuary ranges from 3–5 metres (9.8–16.4 ft). Scanty desert vegetation in the sanctuary is attributed to five factors: salinity at all depths in most areas, scanty rainfall, high velocity of desert winds, shallow soils and undulating topography of its hill region. Thirteen vegetation communities, 32 varieties of trees and 14 varieties of climbers have been recorded. Specifically,

13468-411: The export of carbon fixed in mangroves is important in coastal food webs. Mangrove forests contribute significantly to coastal ecosystems by fostering complex and diverse food webs . The intricate root systems of mangroves create a habitat conducive to the proliferation of microorganisms, crustaceans, and small fish, forming the foundational tiers of the food chain. This abundance of organisms serves as

13616-399: The first refers to the grains and the second to the cement. For example, a limestone consisting mainly of ooids, with a crystalline matrix, would be termed an oosparite. It is helpful to have a petrographic microscope when using the Folk scheme, because it is easier to determine the components present in each sample. Robert J. Dunham published his system for limestone in 1962. It focuses on

13764-573: The food web of the ocean. Mangrove plantations in Vietnam, Thailand, Philippines, and India host several commercially important species of fish and crustaceans. The mangrove food chain extends beyond the marine ecosystem. Coastal bird species inhabit the tidal ecosystems feeding off small marine organisms and wetland insects. Common bird families found in mangroves around the world are egrets , kingfishers , herons , and hornbills , among many others dependent on ecological range. Bird predation plays

13912-400: The forest vegetation types identified in the sanctuary are: dry deciduous scrub, salvadora scrub, desert thorn forest, babul Acacia nilotica forests, tropical Euphorbia scrub, dry savannah type vegetation, – Salvadora association, gorad ( Senegalia senegal ), Zizyphus scrub and Capparis association. The predominant plant species identified are the gorad and the babul; gorad,

14060-572: The formation of distinctive minerals from the silica and clay present in the original limestone. Two major classification schemes, the Folk and Dunham, are used for identifying the types of carbonate rocks collectively known as limestone. Robert L. Folk developed a classification system that places primary emphasis on the detailed composition of grains and interstitial material in carbonate rocks . Based on composition, there are three main components: allochems (grains), matrix (mostly micrite), and cement (sparite). The Folk system uses two-part names;

14208-405: The functional characteristics of root-associated microbial communities in plant growth and biogeochemical cycling. Unraveling functional patterns across the four root compartments holds a great potential for understanding functional mechanisms responsible for mediating root–microbe interactions in support of enhancing mangrove ecosystem functioning. The diversity of bacteria in disturbed mangroves

14356-429: The geologic record are called bioherms . Many are rich in fossils, but most lack any connected organic framework like that seen in modern reefs. The fossil remains are present as separate fragments embedded in ample mud matrix. Much of the sedimentation shows indications of occurring in the intertidal or supratidal zones, suggesting sediments rapidly fill available accommodation space in the shelf or platform. Deposition

14504-402: The habitat of avifauna and flora of the forest; the encroachment for cultivation by farmers is also a major factor that reduces the reserve area and restricts movement of wildlife; cattle grazing and cutting of trees for fuel and other purposes has also caused denudation that affects bird habitats. The conservation measures suggested include preservation of wetland, particularly the water bodies in

14652-402: The health and productivity of mangroves. Many researchers have successfully applied knowledge acquired about plant microbiomes to produce specific inocula for crop protection. Such inocula can stimulate plant growth by releasing phytohormones and enhancing uptake of some mineral nutrients (particularly phosphorus and nitrogen). However, most of the plant microbiome studies have focused on

14800-626: The importance of root-associated bacteria and fungi for mangrove growth and health. Recent studies have investigated the detailed structure of root-associated microbial communities at a continuous fine-scale in other plants, where a microhabitat was divided into four root compartments: endosphere, episphere, rhizosphere, and nonrhizosphere or bulk soil . Moreover, the microbial communities in each compartment have been reported to have unique characteristics. Root exudates selectively enrich adapted microbial populations; however, these exudates were found to exert only marginal impacts on microbes in

14948-434: The last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite , a closely related rock, which contains a high percentage of the mineral dolomite , CaMg(CO 3 ) 2 . Magnesian limestone

15096-492: The last remaining habitats of the cheetah ( Acinonyx jubatus ) in India and are proposed as some of the possible sites for the reintroduction of the species in India. Asiatic cheetah ( Acinonyx jubatus venaticus ) that used to occur here are now locally extinct in India and elsewhere, except a very small critically endangered and fragmented population of last few, estimated to be below 100, thought to be surviving only in

15244-492: The limited fresh water available in salty intertidal soils, mangroves limit the amount of water they lose through their leaves. They can restrict the opening of their stomata (pores on the leaf surfaces, which exchange carbon dioxide gas and water vapor during photosynthesis). They also vary the orientation of their leaves to avoid the harsh midday sun and so reduce evaporation from the leaves. A captive red mangrove grows only if its leaves are misted with fresh water several times

15392-466: The limits of distribution, the formation is represented by scrubby, usually monotypic Avicennia -dominated vegetation, as at Westonport Bay and Corner Inlet, Victoria, Australia. The latter locality is the highest latitude (38° 45'S) at which mangroves occur naturally. The mangroves in New Zealand, which extend as far south as 37°, are of the same type; they start as low forest in the northern part of

15540-533: The local economy. An order dated July 27, 1993 of the Gujarat State Government initially de-notified the Sanctuary, by annulling the earlier notification of 1981 under which Narayan Sarovar had been declared a wildlife sanctuary. It issued a decree which abolished the original sanctuary and established a new one, consisting of 16 disjointed patches. This de-notification had reduced the area of

15688-472: The major limitation to the number of species able to thrive in their habitat. High tide brings in salt water, and when the tide recedes, solar evaporation of the seawater in the soil leads to further increases in salinity. The return of tide can flush out these soils, bringing them back to salinity levels comparable to that of seawater. At low tide, organisms are also exposed to increases in temperature and reduced moisture before being then cooled and flooded by

15836-535: The mangrove species in each listed plant genus and family. Mangrove environments in the Eastern Hemisphere harbor six times as many species of trees and shrubs as do mangroves in the New World. Genetic divergence of mangrove lineages from terrestrial relatives, in combination with fossil evidence, suggests mangrove diversity is limited by evolutionary transition into the stressful marine environment, and

15984-403: The model plant Arabidopsis thaliana and economically important crop plants, such as rice , barley , wheat , maize and soybean . There is less information on the microbiomes of tree species. Plant microbiomes are determined by plant-related factors (e.g., genotype , organ, species, and health status) and environmental factors (e.g., land use, climate, and nutrient availability). Two of

16132-488: The most abundant biological entities on earth, present in virtually all ecosystems. By lysing their hosts, that is, by rupturing their cell membranes, viruses control host abundance and affect the structure of host communities. Viruses also influence their host diversity and evolution through horizontal gene transfer , selection for resistance and manipulation of bacterial metabolisms . Importantly, marine viruses affect local and global biogeochemical cycles through

16280-614: The number of mangrove lineages has increased steadily over the Tertiary with little global extinction. Mangroves are a type of tropical vegetation with some outliers established in subtropical latitudes, notably in South Florida and southern Japan, as well as South Africa, New Zealand and Victoria (Australia). These outliers result either from unbroken coastlines and island chains or from reliable supplies of propagules floating on warm ocean currents from rich mangrove regions. "At

16428-410: The ocean basins, but limestone is rarely preserved in continental slope and deep sea environments. The best environments for deposition are warm waters, which have both a high organic productivity and increased saturation of calcium carbonate due to lower concentrations of dissolved carbon dioxide. Modern limestone deposits are almost always in areas with very little silica-rich sedimentation, reflected in

16576-473: The parent tree. Once germinated, the seedling grows either within the fruit (e.g. Aegialitis , Avicennia and Aegiceras ), or out through the fruit (e.g. Rhizophora , Ceriops , Bruguiera and Nypa ) to form a propagule (a ready-to-go seedling) which can produce its own food via photosynthesis . The mature propagule then drops into the water, which can transport it great distances. Propagules can survive desiccation and remain dormant for over

16724-429: The past few years, bridging the research gap and expanding our knowledge towards the relationship between microbes mainly constituted of bacteria and its nutrient cycles in the mangrove sediment and direct and indirect impacts on mangrove growth and stand-structures as coastal barriers and other ecological service providers. Thus, based on studies by Lai et al.'s systematic review, here they suggest sampling improvements and

16872-927: The plant via root exudates , thus close associations between the plant and microbes are established for their mutual benefits. The taxonomic class level shows that most Proteobacteria were reported to come from Gammaproteobacteria, followed by Deltaproteobacteria and Alphaproteobacteria. The diverse function and the phylogenic variation of Gammaproteobacteria, which consisted of orders such as Alteromonadales and Vibrionales, are found in marine and coastal regions and are high in abundance in mangrove sediments functioning as nutrient recyclers. Members of Deltaproteobacteria found in mangrove soil are mostly sulfur-related, consisting of Desulfobacterales , Desulfuromonadales , Desulfovibrionales , and Desulfarculales among others. Highly diverse microbial communities (mainly bacteria and fungi ) have been found to inhabit and function in mangrove roots. For example, diazotrophic bacteria in

17020-453: The plant was exposed. In a frequently cited concept that has become known as the "sacrificial leaf", salt which does accumulate in the shoot (sprout) then concentrates in old leaves, which the plant then sheds. However, recent research on the Red mangrove Rhizophora mangle suggests that the older, yellowing leaves have no more measurable salt content than the other, greener leaves. Because of

17168-549: The plant-related factors, plant species, and genotypes, have been shown to play significant roles in shaping rhizosphere and plant microbiomes, as tree genotypes and species are associated with specific microbial communities . Different plant organs also have specific microbial communities depending on plant-associated factors (plant genotype, available nutrients, and organ-specific physicochemical conditions) and environmental conditions (associated with aboveground and underground surfaces and disturbances). Mangrove roots harbour

17316-426: The reaction: Fossils are often preserved in exquisite detail as chert. Cementing takes place rapidly in carbonate sediments, typically within less than a million years of deposition. Some cementing occurs while the sediments are still under water, forming hardgrounds . Cementing accelerates after the retreat of the sea from the depositional environment, as rainwater infiltrates the sediment beds, often within just

17464-412: The reduction of the sanctuary area". In August 1995, the Gujarat state legislative assembly taking advantage of the court's reluctance to support the sanctuary approved a reduction in the size of the sanctuary area from 765.79 square kilometres (295.67 sq mi) to 444.23 square kilometres (171.52 sq mi) thus stripping protection from more than 40 per cent of the original protected area of

17612-564: The reintroduction project has been on hold in 2012, after the discovery that Asiatic cheetahs are genetically distinct and have been separated from the South African cheetahs ( Acinonyx jubatus jubatus ) between 32,000 and 67,000 years ago. The sanctuary is generally made up of natural desert thorn forests and grasslands - a mixed forest system comprising dry savannah , desert thorn, tropical euphorbia scrub forest and Salvadora scrub forest, Rann saline scrub and desert dune. In view of

17760-482: The relative purity of most limestones. Reef organisms are destroyed by muddy, brackish river water, and carbonate grains are ground down by much harder silicate grains. Unlike clastic sedimentary rock, limestone is produced almost entirely from sediments originating at or near the place of deposition. Limestone formations tend to show abrupt changes in thickness. Large moundlike features in a limestone formation are interpreted as ancient reefs , which when they appear in

17908-731: The release of substantial amounts of organic carbon and nutrients from hosts and assist microbes in driving biogeochemical cycles with auxiliary metabolic genes (AMGs). It is presumed AMGs augment viral-infected host metabolism and facilitate the production of new viruses. AMGs have been extensively explored in marine cyanophages and include genes involved in photosynthesis, carbon turnover, phosphate uptake and stress response. Cultivation-independent metagenomic analysis of viral communities has identified additional AMGs that are involved in motility, central carbon metabolism, photosystem I, energy metabolism, iron–sulphur clusters, anti-oxidation and sulphur and nitrogen cycling. Interestingly,

18056-457: The rest of the plant. One study found that roots of the Indian mangrove Avicennia officinalis exclude 90% to 95% of the salt in water taken up by the plant, depositing the excluded salt in the cortex of the root. An increase in the production of suberin and in the activity of a gene regulating cytochrome P450 were observed in correlation with an increase in the salinity of the water to which

18204-460: The rock. The Dunham scheme is more useful for hand samples because it is based on texture, not the grains in the sample. A revised classification was proposed by Wright (1992). It adds some diagenetic patterns to the classification scheme. Travertine is a term applied to calcium carbonate deposits formed in freshwater environments, particularly waterfalls , cascades and hot springs . Such deposits are typically massive, dense, and banded. When

18352-439: The sanctuary and maintained that there were around 1200 chinkaras and that the smaller area was more than adequate for them. The new boundaries of the smaller sanctuary were carefully drawn to exclude the rich limestone and mineral-bearing areas. Environment groups contest that cement makers, eager for new sources of limestone, have been the main driving force behind the Gujarat state government's actions. The industry department of

18500-510: The sanctuary area primarily consist of basaltic rocks on the eastern part, tertiary formation in the central part comprising numimulistic limestone and shale bordering the basaltic rocks in south and up to Lakhpat, recent alluvium in a belt of 5–15 kilometres (3.1–9.3 mi) along the coast and scattered coastal sand dunes are on the western boundary. The area is rich in minerals such as limestone in 49 square kilometres (19 sq mi) belt (assessed as 1270 million tonnes) extends from

18648-524: The sanctuary by limestone mining within its vicinity) provided by the Centre for Environment Education (CEE), Ahmedabad which had initially brought the whole issue of de-notification to public light through its media campaign. In March 1995 the Gujarat High Court quashed the government decree, restoring the original sanctuary. But the court refused to comment on the "desirability or otherwise of

18796-451: The sanctuary even before the 1993 decree that had initially abolished it escalating the mining and quarrying. Local forest officials believe that chinkara population is declining in the sanctuary and that their numbers are dwindling because their habitat is being destroyed. Pollution from the power station and the heavy traffic through the protected area also disrupts wildlife. Mining has made the water table salty, driving local villagers out of

18944-401: The sanctuary from765.79 square kilometres (295.67 sq mi) to disjointed ribbons of land totaling only 94.87 square kilometres (36.63 sq mi) in favor of commercial mining interests. The commercially biased court order reduced the area to a mere one-eighth of the original size, with a comment that the area was "substantially in excess of the requirements of a Sanctuary". Following

19092-479: The sanctuary to retain and attract migratory birds, availability and creation of hole-nester by prevention of clearance of dead trees, and attention to globally or nationally threatened species by protecting their habitats; the two species specifically referred are the pied tit (white-napped tit) considered endemic to India and the MacQueen's bustard ( houbara bustard ); in this context, the yellow-crowned woodpecker

19240-458: The sanctuary. The flowering plants listed in the sanctuary include 252 species, important ones being desi baval, gorad, hermo, ber , pilu , thor, gando baval, gugal, ingorio, kerdo and cariso . The desert ecosystem of the sanctuary has been affected by several factors. Some of the key factors identified are: restricting the reserve area and allocating limestone areas for mining, which not only encroached on this precious forest but also disturbed

19388-411: The sediment due to the tidal flushing of mangrove forests. Termites play an important role in the formation of peat from mangrove materials. They process fallen leaf litter , root systems and wood from mangroves into peat to build their nests, and stabilise the chemistry of this peat that represents approximately 2% of above ground carbon storage in mangroves. As the nests are buried over time this carbon

19536-479: The sediments increases. Chemical compaction takes place by pressure solution of the sediments. This process dissolves minerals from points of contact between grains and redeposits it in pore space, reducing the porosity of the limestone from an initial high value of 40% to 80% to less than 10%. Pressure solution produces distinctive stylolites , irregular surfaces within the limestone at which silica-rich sediments accumulate. These may reflect dissolution and loss of

19684-662: The sediments of the ocean floor abruptly transition from carbonate ooze rich in foraminifera and coccolith remains ( Globigerina ooze) to silicic mud lacking carbonates. In rare cases, turbidites or other silica-rich sediments bury and preserve benthic (deep ocean) carbonate deposits. Ancient benthic limestones are microcrystalline and are identified by their tectonic setting. Fossils typically are foraminifera and coccoliths. No pre-Jurassic benthic limestones are known, probably because carbonate-shelled plankton had not yet evolved. Limestones also form in freshwater environments. These limestones are not unlike marine limestone, but have

19832-465: The soil like straws for breathing. These "breathing tubes" typically reach heights of up to 30 cm (12 in), and in some species, over 3 m (9.8 ft). The roots also contain wide aerenchyma to facilitate transport within the plants. Because the soil is perpetually waterlogged, little free oxygen is available. Anaerobic bacteria liberate nitrogen gas, soluble ferrum (iron), inorganic phosphates , sulfides , and methane , which make

19980-503: The soil much less nutritious. Pneumatophores ( aerial roots ) allow mangroves to absorb gases directly from the atmosphere, and other nutrients such as iron, from the inhospitable soil. Mangroves store gases directly inside the roots, processing them even when the roots are submerged during high tide. Red mangroves exclude salt by having significantly impermeable roots that are highly suberised (impregnated with suberin ), acting as an ultrafiltration mechanism to exclude sodium salts from

20128-412: The south Saran Nani village to Lakhpat, lignite in a belt of 32.5 square kilometres (12.5 sq mi) (15 million tonnes) and bentonite; lignite and bentonite are being mined close to Panandhro and Saran villages, while the mining of limestone is yet to begin. Sandy alluvium, clay and black loam are the soil types identified in the sanctuary area. However, vegetation in the central area of the sanctuary

20276-757: The species chosen. The International Day for the Conservation of the Mangrove Ecosystem is celebrated every year on 26 July. Etymology of the English term mangrove can only be speculative and is disputed. The term may have come to English from the Portuguese mangue or the Spanish mangle . Further back, it may be traced to South America and Cariban and Arawakan languages such as Taíno . Other possibilities include

20424-460: The state has been receiving several applications to build cement factories in the de-notified area. The Gujarat state assembly also stressed that Gujarat with its poor power supply cannot afford to ignore its brown coal deposits. The first lignite-fueled power generation station was built inside the sanctuary in 1991 and the second is now planned in Akri. Some miners had moved inside the boundaries of

20572-435: The tide. Thus, for a plant to survive in this environment, it must tolerate broad ranges of salinity, temperature, and moisture, as well as several other key environmental factors—thus only a select few species make up the mangrove tree community. About 110 species are considered mangroves, in the sense of being trees that grow in such a saline swamp, though only a few are from the mangrove plant genus, Rhizophora . However,

20720-767: The tropical conditions of variable salinity, tidal range (inundation), anaerobic soils, and intense sunlight. Plant biodiversity is generally low in a given mangrove. The greatest biodiversity of mangroves occurs in Southeast Asia , particularly in the Indonesian archipelago . The red mangrove ( Rhizophora mangle ) survives in the most inundated areas, props itself above the water level with stilt or prop roots and then absorbs air through lenticels in its bark. The black mangrove ( Avicennia germinans ) lives on higher ground and develops many specialized root-like structures called pneumatophores , which stick up out of

20868-579: The vicinity of mangrove roots could perform biological nitrogen fixation , which provides 40–60% of the total nitrogen required by mangroves; the soil attached to mangrove roots lacks oxygen but is rich in organic matter, providing an optimal microenvironment for sulfate-reducing bacteria and methanogens , ligninolytic , cellulolytic , and amylolytic fungi are prevalent in the mangrove root environment; rhizosphere fungi could help mangroves survive in waterlogged and nutrient-restricted environments. These studies have provided increasing evidence to support

21016-533: The water by photosynthesis and thereby decreasing the solubility of calcium carbonate. Limestone shows the same range of sedimentary structures found in other sedimentary rocks. However, finer structures, such as lamination , are often destroyed by the burrowing activities of organisms ( bioturbation ). Fine lamination is characteristic of limestone formed in playa lakes , which lack the burrowing organisms. Limestones also show distinctive features such as geopetal structures , which form when curved shells settle to

21164-553: The water. Although ooids likely form through purely inorganic processes, the bulk of CaCO 3 precipitation in the oceans is the result of biological activity. Much of this takes place on carbonate platforms . The origin of carbonate mud, and the processes by which it is converted to micrite, continue to be a subject of research. Modern carbonate mud is composed mostly of aragonite needles around 5 μm (0.20 mils) in length. Needles of this shape and composition are produced by calcareous algae such as Penicillus , making this

21312-642: The west. There are records of A. germinans and Rhizophora mangle for Bermuda, presumably supplied by the Gulf Stream. In southern Japan, Kandelia obovata occurs to about 31 °N (Tagawa in Hosakawa et al., 1977, but initially referred to as K. candel )." Mangrove forests , also called mangrove swamps or mangals , are found in tropical and subtropical tidal areas. Areas where mangroves occur include estuaries and marine shorelines. The intertidal existence to which these trees are adapted represents

21460-403: The world's subtropical and tropical coastlines. Mangroves are one of the most productive and ecologically important ecosystems on earth. The rates of primary production of mangroves equal those of tropical humid evergreen forests and coral reefs. As a globally relevant component of the carbon cycle, mangroves sequester approximately 24 million metric tons of carbon each year. Most mangrove carbon

21608-550: The world. In 2018, the Global Mangrove Watch Initiative released a new global baseline which estimates the total mangrove forest area of the world as of 2010 at 137,600 km (53,100 sq mi), spanning 118 countries and territories. A 2022 study on losses and gains of tidal wetlands estimates a 3,700 km (1,400 sq mi) net decrease in global mangrove extent from 1999 to 2019. Mangrove loss continues due to human activity, with

21756-415: Was established in 2006 with the objective of providing important information to the public about the sanctuary. Even 30–35 hutments were constructed as part of the centre. It was inaugurated with a lot of fanfare when the 'Kutch Utsav' was organized here. Unfortunately, the centre has remained neglected without any staff to man it (funds constraint is mooted as one of the reasons). The forest officials say that

21904-416: Was likely deposited in pore space between grains, suggesting a high-energy depositional environment that removed carbonate mud. Recrystallized sparite is not diagnostic of depositional environment. Limestone outcrops are recognized in the field by their softness (calcite and aragonite both have a Mohs hardness of less than 4, well below common silicate minerals) and because limestone bubbles vigorously when

#183816