Current Search: Florida (x)
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Title
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A literature review of ocean acidification’s effect on coral calcification rates and skeletal growth.
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Name/Creator
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Camden, Lauren
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Abstract/Description
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Ocean acidification is one of many threats to marine life as a result of increasing levels of atmospheric carbon dioxide being absorbed by ocean water. Anthropogenic levels of carbon dioxide have been rising dramatically in the atmosphere since the onset of the Industrial Revolution, with a sharp escalation occurring due to practices such as the burning of fossil fuels. The ocean acts as a carbon sink for atmospheric CO2, absorbing a large portion of it. This process causes a chemical...
Show moreOcean acidification is one of many threats to marine life as a result of increasing levels of atmospheric carbon dioxide being absorbed by ocean water. Anthropogenic levels of carbon dioxide have been rising dramatically in the atmosphere since the onset of the Industrial Revolution, with a sharp escalation occurring due to practices such as the burning of fossil fuels. The ocean acts as a carbon sink for atmospheric CO2, absorbing a large portion of it. This process causes a chemical reaction that progressively lowers the average pH of oceans globally. When a carbon dioxide molecule is absorbed into sea water, two positively charged ions are produced. As pH value is a measurement of hydrogen ion concentration in any given solution, these added hydrogen ions effectively lower the pH of the ocean and causes it to be more acidic. Since these hydrogen ions are positively charged, they to interact with the negatively charged bases already present in the ocean. One of these bases is CaCO3, or the carbonate ion. Carbonate is essential to calcifying marine organisms, who use this ion to build and maintain their shells and skeletons. However, as atmospheric carbon dioxide levels increase and the resulting chemical reactions occur, the ocean’s carbonate saturation decreases. Coral is one such calcifying organism that essential to the aquatic ecosystem in a number of ways, most of which can be attributed to the fact that coral reefs are one of the planet’s most biodiverse ecosystems despite inhabiting only a very small portion of the ocean. With this process occurring at accumulative speeds, how will ocean acidification affect the calcification rates- and therefore the growth and development- of coral in the coming years worldwide? Several studies have confirmed the relationship between increased carbon dioxide levels and the resulting decreased calcification levels and structural deformities present in coral reefs. In 2005 Langdon et al published a study that tested coral calcification rates with varying rates of carbon dioxide saturation in ocean water. Specimens of Porites compressa (finger coral) and Montipora verucosa (rice coral) were collected off the coast of Hawaii and placed in an offshore experimental flume where a series of incubations were performed in Summer 1999 and Winter 2000. From August to September 1999, eighteen incubations were performed with ambient conditions and nine incubations were performed with pCO2 levels at 1.7 times what ambient conditions were. A second round of fifteen incubations were performed from January to February 2000. Six incubations were done at an ambient pCO2, two were done at 1.4 times, and six were done at 2.0 times ambient conditions. Calcification rates for all incubations were calculated through statistical analysis. As a result, calcification decreased 26%, 40%, and 80% respectively to increased pCO2. Another such study was conducted by Langdon et al again in 2013, this time in the Florida Bay. Samples of Siderastrea radians (shallow starlet coral) and Solenastrea hyades (smooth star coral) were collected near Peterson Key and attached to cinderblocks with sensors logging environmental data such as pH and temperature at thirty-minute intervals. A random subset of these corals was incubated in situ and given a treatment regime designed to simulate increased ocean acidification conditions. This treatment lowered pH value in the incubation chambers by 0.1 to 0.2 units. Calcification rates of the incubated coral samples were determined through statistical analysis. Coral samples that experienced a 0.1 unit drop in pH value experienced decreased calcification rates of 50% and coral samples that experiences a 0.2 unit drop in pH value experienced a decreased calcification rate of 52%. These studies both exemplified the strong correlation that exists between pCO2 present, increased acidity in ocean water, and decreased calcification rates of coral. In 2016, Foster et al published a study that demonstrated the structural deformities coral experience as a result of this calcification reduct.
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Date Issued
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2020-06-15
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Identifier
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BC742
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC742
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Title
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African Mask.
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Abstract/Description
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This is a Songye mask. The Songye people live in Democratic Republic of Congo. They are a relatively small tribe with a central chief and many secret societies. This mask or kifewebe, as masks are called in the Songye language, is of a male figure. This is determined by the center crest on its head. It represents a spirit and bears striations which is one of the chief differentiators of Songye masks. A mask like this would have been used by the kifewebe society to ward off evil, avert...
Show moreThis is a Songye mask. The Songye people live in Democratic Republic of Congo. They are a relatively small tribe with a central chief and many secret societies. This mask or kifewebe, as masks are called in the Songye language, is of a male figure. This is determined by the center crest on its head. It represents a spirit and bears striations which is one of the chief differentiators of Songye masks. A mask like this would have been used by the kifewebe society to ward off evil, avert disaster and heal the sick. When worn in dances, it serves the dancer for its connotation of aggression to help the chief maintain order and control. This mask is believed to embody supernatural forces and the magic it carries is decided by the size of its crest. The white color of the striations symbolizes peace and purity while the red could mean any of danger, fire, blood, evil, courage or fortitude. Songye masks are easily identified by their striations and their shapes. The eyes, noses and mouths are carved in high relief. Often, the lips form star-shaped puckers to give the masks the impression of whistling or pouting.
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Identifier
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BC004, 2014
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Format
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Image (JPEG2000)
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PURL
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http://purl.flvc.org/broward/fd/BC004
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Title
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AGRRA protocols and coral reef health in the Caribbean.
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Name/Creator
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Quintana, Arely
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Abstract/Description
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The objective of The Atlantic and Gulf Rapid Reef Assessment (AGRRA) coral monitoring is to assess the size and overall condition of corals ≥ 4 cm to help evaluate important structural and functional attributes of tropical western Atlantic coral reefs. Data collected can provide information representative of large areas, like shelves, islands, countries or ecoregions. The coral monitoring surveys can be performed by snorkeling (
Show moreThe objective of The Atlantic and Gulf Rapid Reef Assessment (AGRRA) coral monitoring is to assess the size and overall condition of corals ≥ 4 cm to help evaluate important structural and functional attributes of tropical western Atlantic coral reefs. Data collected can provide information representative of large areas, like shelves, islands, countries or ecoregions. The coral monitoring surveys can be performed by snorkeling (< 1.5 m), but SCUBA is now recommended for most assessments with diver expertise ranging from novice to highly trained. Survey sites should be chosen randomly within a geomorphic zone of a reef on an insular or continental shelf within one of twelve marine shelf ecoregions of the Tropical Northwestern province of the Tropical Atlantic biogeographic realm. The spatial extent of a site is about 200 m x 200 m and zones of maximum reef development are highly recommended. Recording of exact location using GPS is critical for data quality and consistency. Surveys are completed to assess coral health, recruitments, size, and species. Although single metrics are insufficient to measure whole coral system health due to the highly dynamic nature of reefs, the information collected can indirectly measure environmental quality of the reef and assist in understanding the effects of local and regional stressors. The use of trained volunteer divers whether amateur or professional provides a wealth of information in a cost friendly manner and the data collected from over 3,000 surveys is available in an open-access public database. Information collected from monitoring surveys has become a key source of scientific data used in other research programs, reef policies, legislation, management and conservation.
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Date Issued
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2021-04-21
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Identifier
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BC3355
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC3355
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Title
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Asian Lotus Shoe.
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Abstract/Description
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Foot binding (also known as "Lotus feet") is the custom of applying painfully tight binding to the feet of young girls to prevent further growth. The practice possibly originated among upper-class court dancers during the Five Dynasties and Ten Kingdoms period in Imperial China (10th or 11th century). Foot binding became popular as a means of displaying status (women from wealthy families who did not need them to work could afford to have their feet bound) and was correspondingly adopted as a...
Show moreFoot binding (also known as "Lotus feet") is the custom of applying painfully tight binding to the feet of young girls to prevent further growth. The practice possibly originated among upper-class court dancers during the Five Dynasties and Ten Kingdoms period in Imperial China (10th or 11th century). Foot binding became popular as a means of displaying status (women from wealthy families who did not need them to work could afford to have their feet bound) and was correspondingly adopted as a symbol of beauty in Chinese culture. Shoe for bound foot. Cloth, with black edging, purple cloth tape; embroidered floral/swastika design; pink tapes for securing shoe; broad cloth piece sewn to inside heel; reinforced arched sole with blue/white/red stripes and floral painted design.
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Identifier
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BC005, 1928
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Format
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Image (JPEG2000)
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PURL
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http://purl.flvc.org/broward/fd/BC005
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Title
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Blue Morpho Butterfly.
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Abstract/Description
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The blue morpho butterfly’s wings are bright blue, edged with black and brown. The blue morpho is among the largest butterflies in the world, with wings spanning from five to eight inches. Their vivid, iridescent blue coloring is a result of the microscopic scales on the backs of their wings, which reflect light. The underside of the morpho’s wings, on the other hand, is a dull brown color with many eyespots.
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Date Issued
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1996
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Identifier
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BC040, 1906
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Format
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Image (JPEG2000)
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PURL
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http://purl.flvc.org/broward/fd/BC040
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Title
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Delaware state soil - Greenwich.
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Name/Creator
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Gazdick, Kaitlin
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Abstract/Description
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The predominate soil order in Delaware is Ultisols. They are located in mostly humid, temperate, and tropical areas that are in older and more stable parts of the world. An accumulation of clay can be found on the top layer. They consist of weathered, acid forest soils, low in calcium, magnesium, and potassium. These elements are present in soil as ions forming cation exchange capacity that is often reduced due to leaching and take up 9.2 percent of the total United States land area. The...
Show moreThe predominate soil order in Delaware is Ultisols. They are located in mostly humid, temperate, and tropical areas that are in older and more stable parts of the world. An accumulation of clay can be found on the top layer. They consist of weathered, acid forest soils, low in calcium, magnesium, and potassium. These elements are present in soil as ions forming cation exchange capacity that is often reduced due to leaching and take up 9.2 percent of the total United States land area. The state soil of Delaware is Greenwich, and it is the most significant and prevalent soil in the state. Greenwich is located on uplands of the coastal plain and consists of 123,000+ acres and takes up 9.4 percent of land in Delaware. The parent material is sandy alluvial sediments, transported by water, from the Atlantic Coastal Plain overlain with deposits high silt bothwind-blown, and water transported sediment. The warm humid climate in which Greenwich developed, causes leaching due to abundant rainfall. Leaves, twigs, roots, and other plant material on the surface of pine forests degrade into the soil. The soil horizon is described as having a topsoil of brown loam that is 10 inches thick brown loam. The upper subsoil is strong brown loam, and the lower subsoil is yellowish brown sandy loam. The substratum is yellowish brown coarse sand stratified with dark yellowish brown loamy sand. Greenwich is a productive soil used for crops such as vegetables and forest products. It is also often used for construction and recreational development.
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Date Issued
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2021-04-21
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Identifier
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BC3352
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC3352
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Title
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Five years' hunting adventures in South Africa : being an account of sport with the lion, elephant, buffalo, rhinoceros, camelopard, ostrich, hippopotamus, wildebest, koodoo, hyaena, &c., &c.
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Name/Creator
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Gordon-Cumming, Roualeyn
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Date Issued
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[1892?]
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Identifier
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BC065, fiveyearshunting1892roua
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC065
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Title
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Generation of tsunamis from earthquakes: a literature review.
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Name/Creator
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Naum, Miranda
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Abstract/Description
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Tsunamis are some of the most incredible yet devastating forces of mother nature. Their sheer and immense power is something of fascination. Earthquakes are primarily responsible for the generation of these massive waves. But what exactly is the link between earthquakes and tsunamis? Tsunamis are a series of ocean waves produced by the displacement of great volumes of water. The displacement of water is typically caused by submarine earthquakes. These earthquakes deform the seafloor, causing...
Show moreTsunamis are some of the most incredible yet devastating forces of mother nature. Their sheer and immense power is something of fascination. Earthquakes are primarily responsible for the generation of these massive waves. But what exactly is the link between earthquakes and tsunamis? Tsunamis are a series of ocean waves produced by the displacement of great volumes of water. The displacement of water is typically caused by submarine earthquakes. These earthquakes deform the seafloor, causing the sudden dislocation of a few to tens of cubic kilometers of water. Approximately 80% of tsunamis are the result of underwater earthquakes. Modern methods of studying the relationship between earthquakes and tsunamis involve the use of virtual laboratories, computational models, physical models, kinematic models, and dislocation models. Large tsunamis require substantial parent earthquakes because more than 96% of their energy is stored in the ocean. The resulting tsunami is a means of releasing energy. The larger the earthquake, the larger the proceeding tsunami will be. Though less than 1% of an earthquake’s energy is actually converted into tsunamis, the energy is capable of generating deadly and catastrophic tsunamis. Further investigation may be proposed to analyze other causes of tsunamis, such as submarine landslides.
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Date Issued
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2021-04-21
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Identifier
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BC3359
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC3359
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Title
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How will the predicted ocean temperatures of 2100, impact larval development of Lobatus (Strombus) gigas in the Caribbean region?.
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Name/Creator
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Pollard, Madison Jane
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Abstract/Description
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In the Caribbean region, calcareous shelled organisms are at risk of inhibited larval development (e.g., shell growth and mortality) at high ocean temperatures. Given predicted sea-surface temperatures due to global climate change for the year 2100 (by the IPCC and NOAA) researchers are predicting at what temperatures these changes could affect larval development of Queen conch, Lobatus (Strombus) gigas. Carbon emissions from human activities (e.g., burning of fossil fuels) are affecting...
Show moreIn the Caribbean region, calcareous shelled organisms are at risk of inhibited larval development (e.g., shell growth and mortality) at high ocean temperatures. Given predicted sea-surface temperatures due to global climate change for the year 2100 (by the IPCC and NOAA) researchers are predicting at what temperatures these changes could affect larval development of Queen conch, Lobatus (Strombus) gigas. Carbon emissions from human activities (e.g., burning of fossil fuels) are affecting marine organisms at multiple trophic levels due to ocean warming and acidification. L. gigas was abundant in their geographic range of the Caribbean Sea, the Gulf of Mexico, and around Bermuda, now with a combination of overharvesting and global climate change, conchs are candidates for the Endangered Species Act. As CO2 increases in the ocean, carbonate for calcium carbonate production decreases. L. gigas will use more energy to produce their shells (stunting growth rates) or opt for weaker shells. Researchers (Aranda and Manzano) reared L.gigas eggs from hatchling to settlement under five temperatures (28, 28.5, 29, 29.5, 30℃) to assess growth and development. At 30 ℃ larvae experienced faster growth rates, but survival was low (23%). While at 28 ℃ larvae had the highest survival (35%). Temperature seemed to have more of a direct impact on earlier stages of larvae of L. gigas than those closest to settlement. Queen conchs are economically important for their commercial value, being the second largest fishery in the Caribbean. Ocean warming and acidification would cause a decrease in harvest, changing prices for consumers. Urgent action against reducing greenhouse gas emissions must be taken. The Caribbean can mitigate contribution to greenhouse gases by renewable energy since it is an area that has great potential for hydro-electric, geothermal, wind and solar energy. This in turn could reduce the impacts to L. gigas larval development.
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Date Issued
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2021-04-21
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Identifier
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BC3356
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC3356
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Title
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Miamian Ohio’s state soil.
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Name/Creator
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Williams, Kristin Anne
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Abstract/Description
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Originally named part of the Miami soil series, in 1969 Miamian soil was separated. Miamian is found in the central lowland till plains in Ohio, Indiana and Illinois. It is formed from Wisconsinan till in the till plains and moraines under deciduous hardwood forests. Miamian is an Alfisol, and a fine, mixed, active, mesic Oxyaquic Hapludalfs. It is composed of moderately well drained, loess or silty material and underlying loamy till. It has a moderate amount of organic matter and is well...
Show moreOriginally named part of the Miami soil series, in 1969 Miamian soil was separated. Miamian is found in the central lowland till plains in Ohio, Indiana and Illinois. It is formed from Wisconsinan till in the till plains and moraines under deciduous hardwood forests. Miamian is an Alfisol, and a fine, mixed, active, mesic Oxyaquic Hapludalfs. It is composed of moderately well drained, loess or silty material and underlying loamy till. It has a moderate amount of organic matter and is well leached of calcium carbonate. The A horizon contains: Silt 39-49%, 11-18% clay, 38-46% sand. The typical pedon contains the following horizons: an Ap (brown silt loam), 2Bt1 (clay loam), 2Bt2 (clay loam), 2Bt3 (clay), 2BC (loam), and a 2Cd (loam). Other horizons can be found but are not always present. Miamian is named as Ohio’s state soil because of the important role it plays in agriculture. Almost all this soil series has been converted to broad acreage agriculture and makes highly productive farmland. Corn, soybeans, winter wheat, and oats are the prime crops, while forages, pastures and hardwood forest trees are more common on steeper slopes. Miamian soil is usually found on convex slopes and has good rainfall, both of which make it highly suspectable to erosion. The use of no till planting, cover crops and crop rotation have all been used to prevent erosion. The A horizon is often to acidic 5.4 to grow corn, so liming agents are frequently used to bring up the pH closer to 6. Miamian soil is well drained and is not suited for filtering liquids, such as with septic tanks.
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Date Issued
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2020-06-15
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Identifier
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BC741
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Format
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Document (PDF)
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PURL
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http://purl.flvc.org/broward/fd/BC741
Pages