Relationship between coral distributions and physical variables in Amitori Bay, Iriomote Island, Japan
The relationship between coral distributions and physical variables was investigated in Amitori Bay, Iriomote Island, Japan. Field observations were conducted to obtain data on coral distributions, sea temperature, sea salinity, wind speed, and river flow rate. The observed data were then used in oc...
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Veröffentlicht in: | Journal of geophysical research. Oceans 2014-12, Vol.119 (12), p.8336-8356 |
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creator | Shimokawa, Shinya Murakami, Tomokazu Ukai, Akiyuki Kohno, Hiroyoshi Mizutani, Akira Nakase, Kouta |
description | The relationship between coral distributions and physical variables was investigated in Amitori Bay, Iriomote Island, Japan. Field observations were conducted to obtain data on coral distributions, sea temperature, sea salinity, wind speed, and river flow rate. The observed data were then used in ocean and wave model numerical simulations and soil particle tracking analysis to obtain the spatial and temporal distributions of wave height and the numbers of soil particles. The main results of this study indicate that wave height and the number of soil particles have a significant correlation with coral distribution. Higher wave heights result in greater coverage of tabular coral and lower coverage of branching coral. A greater number of soil particles relates to lesser coverage of tabular coral. On the contrary, the number of soil particles is not correlated with branching coral coverage. The potential habitats for tabular corals largely depend on the species. Acropora hyacinthus is distributed in conditions with low numbers of soil particles, A. digitifera is distributed in conditions with low numbers of soil particles and high wave heights, and A. millepora is distributed in conditions with high numbers of soil particles and low wave heights. Averages of diversity index of the coral types at the mouth and inner parts of the bay are lower than average of the whole region, but average of diversity index at the intermediate part of the bay with the intermediate physical disturbances is higher than it, which seems to support the intermediate disturbance hypothesis.
Key Points:
Relationship between coral distribution and physical variable was investigated
Wave and soil particles have a significant correlation with coral distribution
Analysis of diversity index supports the intermediate disturbance hypothesis |
doi_str_mv | 10.1002/2014JC010307 |
format | Article |
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Key Points:
Relationship between coral distribution and physical variable was investigated
Wave and soil particles have a significant correlation with coral distribution
Analysis of diversity index supports the intermediate disturbance hypothesis</description><identifier>ISSN: 2169-9275</identifier><identifier>EISSN: 2169-9291</identifier><identifier>DOI: 10.1002/2014JC010307</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Bioavailability ; Computer simulation ; coral life form ; coral species ; Corals ; Correlation ; Correlation analysis ; Distribution ; Disturbances ; diversity index ; field observation ; Flow rates ; Flow velocity ; Freshwater ; Geophysics ; Hypotheses ; intermediate disturbance hypothesis ; Islands ; Marine ; Mathematical models ; Mouth ; numerical simulation ; Numerical simulations ; Oceans ; Particle tracking ; River flow ; Rivers ; Salinity ; Salinity effects ; Soil ; Soil (material) ; Soil analysis ; Soil investigations ; Soil particles ; Soils ; Spatial distribution ; Temperature ; Temperature effects ; Wave height ; Wind speed</subject><ispartof>Journal of geophysical research. Oceans, 2014-12, Vol.119 (12), p.8336-8356</ispartof><rights>2014. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2014JC010307$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2014JC010307$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,27903,27904,45553,45554,46387,46811</link.rule.ids></links><search><creatorcontrib>Shimokawa, Shinya</creatorcontrib><creatorcontrib>Murakami, Tomokazu</creatorcontrib><creatorcontrib>Ukai, Akiyuki</creatorcontrib><creatorcontrib>Kohno, Hiroyoshi</creatorcontrib><creatorcontrib>Mizutani, Akira</creatorcontrib><creatorcontrib>Nakase, Kouta</creatorcontrib><title>Relationship between coral distributions and physical variables in Amitori Bay, Iriomote Island, Japan</title><title>Journal of geophysical research. Oceans</title><addtitle>J. Geophys. Res. Oceans</addtitle><description>The relationship between coral distributions and physical variables was investigated in Amitori Bay, Iriomote Island, Japan. Field observations were conducted to obtain data on coral distributions, sea temperature, sea salinity, wind speed, and river flow rate. The observed data were then used in ocean and wave model numerical simulations and soil particle tracking analysis to obtain the spatial and temporal distributions of wave height and the numbers of soil particles. The main results of this study indicate that wave height and the number of soil particles have a significant correlation with coral distribution. Higher wave heights result in greater coverage of tabular coral and lower coverage of branching coral. A greater number of soil particles relates to lesser coverage of tabular coral. On the contrary, the number of soil particles is not correlated with branching coral coverage. The potential habitats for tabular corals largely depend on the species. Acropora hyacinthus is distributed in conditions with low numbers of soil particles, A. digitifera is distributed in conditions with low numbers of soil particles and high wave heights, and A. millepora is distributed in conditions with high numbers of soil particles and low wave heights. Averages of diversity index of the coral types at the mouth and inner parts of the bay are lower than average of the whole region, but average of diversity index at the intermediate part of the bay with the intermediate physical disturbances is higher than it, which seems to support the intermediate disturbance hypothesis.
Key Points:
Relationship between coral distribution and physical variable was investigated
Wave and soil particles have a significant correlation with coral distribution
Analysis of diversity index supports the intermediate disturbance hypothesis</description><subject>Bioavailability</subject><subject>Computer simulation</subject><subject>coral life form</subject><subject>coral species</subject><subject>Corals</subject><subject>Correlation</subject><subject>Correlation analysis</subject><subject>Distribution</subject><subject>Disturbances</subject><subject>diversity index</subject><subject>field observation</subject><subject>Flow rates</subject><subject>Flow velocity</subject><subject>Freshwater</subject><subject>Geophysics</subject><subject>Hypotheses</subject><subject>intermediate disturbance hypothesis</subject><subject>Islands</subject><subject>Marine</subject><subject>Mathematical models</subject><subject>Mouth</subject><subject>numerical simulation</subject><subject>Numerical simulations</subject><subject>Oceans</subject><subject>Particle tracking</subject><subject>River flow</subject><subject>Rivers</subject><subject>Salinity</subject><subject>Salinity effects</subject><subject>Soil</subject><subject>Soil (material)</subject><subject>Soil analysis</subject><subject>Soil investigations</subject><subject>Soil particles</subject><subject>Soils</subject><subject>Spatial distribution</subject><subject>Temperature</subject><subject>Temperature effects</subject><subject>Wave height</subject><subject>Wind speed</subject><issn>2169-9275</issn><issn>2169-9291</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkU1LAzEQhhdRULQ3f0DAiwermXxujrpobS0K4tctZLdZjG5312Rr7b83tVLEgziXGZjnHd7hTZJ9wMeAMTkhGNgow4AplhvJDgGh-ooo2FzPkm8nvRBecKwUUsbUTlLe2sp0rqnDs2tRbru5tTUqGm8qNHGh8y6ffa2RqSeofV4EV8TVu_HO5JUNyNXodOq6xjt0ZhZHaOhdM206i4ahipIjNDKtqfeSrdJUwfa--25yf3F-l132xzeDYXY67htBokfGVQFUYcooCAZFLpgseUFUbssJiDyfMFqUFkhJU8N4XlLJVBkRblOFJaG7yeHqbuubt5kNnZ66UNgqWrHNLGgQAmMuCJf_QDkTqcDAI3rwC31pZr6Oj2hQICXjQrI_KcEEJ0DpkqIrau4qu9Ctd1PjFxqwXqaof6aoR4PbjGAlVVT1V6oYif1Yq4x_1UJSyfXj9UBjlT1lV_RB39FPUXidlw</recordid><startdate>201412</startdate><enddate>201412</enddate><creator>Shimokawa, Shinya</creator><creator>Murakami, Tomokazu</creator><creator>Ukai, Akiyuki</creator><creator>Kohno, Hiroyoshi</creator><creator>Mizutani, Akira</creator><creator>Nakase, Kouta</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>201412</creationdate><title>Relationship between coral distributions and physical variables in Amitori Bay, Iriomote Island, Japan</title><author>Shimokawa, Shinya ; Murakami, Tomokazu ; Ukai, Akiyuki ; Kohno, Hiroyoshi ; Mizutani, Akira ; Nakase, Kouta</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a6269-459c13903431641cb647f5c29befd16bbd43cfe12f38a45bf3749f7f55e890723</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Bioavailability</topic><topic>Computer simulation</topic><topic>coral life form</topic><topic>coral species</topic><topic>Corals</topic><topic>Correlation</topic><topic>Correlation analysis</topic><topic>Distribution</topic><topic>Disturbances</topic><topic>diversity index</topic><topic>field observation</topic><topic>Flow rates</topic><topic>Flow velocity</topic><topic>Freshwater</topic><topic>Geophysics</topic><topic>Hypotheses</topic><topic>intermediate disturbance hypothesis</topic><topic>Islands</topic><topic>Marine</topic><topic>Mathematical models</topic><topic>Mouth</topic><topic>numerical simulation</topic><topic>Numerical simulations</topic><topic>Oceans</topic><topic>Particle tracking</topic><topic>River flow</topic><topic>Rivers</topic><topic>Salinity</topic><topic>Salinity effects</topic><topic>Soil</topic><topic>Soil (material)</topic><topic>Soil analysis</topic><topic>Soil investigations</topic><topic>Soil particles</topic><topic>Soils</topic><topic>Spatial distribution</topic><topic>Temperature</topic><topic>Temperature effects</topic><topic>Wave height</topic><topic>Wind speed</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shimokawa, Shinya</creatorcontrib><creatorcontrib>Murakami, Tomokazu</creatorcontrib><creatorcontrib>Ukai, Akiyuki</creatorcontrib><creatorcontrib>Kohno, Hiroyoshi</creatorcontrib><creatorcontrib>Mizutani, Akira</creatorcontrib><creatorcontrib>Nakase, Kouta</creatorcontrib><collection>Istex</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of geophysical research. Oceans</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Shimokawa, Shinya</au><au>Murakami, Tomokazu</au><au>Ukai, Akiyuki</au><au>Kohno, Hiroyoshi</au><au>Mizutani, Akira</au><au>Nakase, Kouta</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Relationship between coral distributions and physical variables in Amitori Bay, Iriomote Island, Japan</atitle><jtitle>Journal of geophysical research. Oceans</jtitle><addtitle>J. Geophys. Res. Oceans</addtitle><date>2014-12</date><risdate>2014</risdate><volume>119</volume><issue>12</issue><spage>8336</spage><epage>8356</epage><pages>8336-8356</pages><issn>2169-9275</issn><eissn>2169-9291</eissn><abstract>The relationship between coral distributions and physical variables was investigated in Amitori Bay, Iriomote Island, Japan. Field observations were conducted to obtain data on coral distributions, sea temperature, sea salinity, wind speed, and river flow rate. The observed data were then used in ocean and wave model numerical simulations and soil particle tracking analysis to obtain the spatial and temporal distributions of wave height and the numbers of soil particles. The main results of this study indicate that wave height and the number of soil particles have a significant correlation with coral distribution. Higher wave heights result in greater coverage of tabular coral and lower coverage of branching coral. A greater number of soil particles relates to lesser coverage of tabular coral. On the contrary, the number of soil particles is not correlated with branching coral coverage. The potential habitats for tabular corals largely depend on the species. Acropora hyacinthus is distributed in conditions with low numbers of soil particles, A. digitifera is distributed in conditions with low numbers of soil particles and high wave heights, and A. millepora is distributed in conditions with high numbers of soil particles and low wave heights. Averages of diversity index of the coral types at the mouth and inner parts of the bay are lower than average of the whole region, but average of diversity index at the intermediate part of the bay with the intermediate physical disturbances is higher than it, which seems to support the intermediate disturbance hypothesis.
Key Points:
Relationship between coral distribution and physical variable was investigated
Wave and soil particles have a significant correlation with coral distribution
Analysis of diversity index supports the intermediate disturbance hypothesis</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2014JC010307</doi><tpages>21</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Bioavailability Computer simulation coral life form coral species Corals Correlation Correlation analysis Distribution Disturbances diversity index field observation Flow rates Flow velocity Freshwater Geophysics Hypotheses intermediate disturbance hypothesis Islands Marine Mathematical models Mouth numerical simulation Numerical simulations Oceans Particle tracking River flow Rivers Salinity Salinity effects Soil Soil (material) Soil analysis Soil investigations Soil particles Soils Spatial distribution Temperature Temperature effects Wave height Wind speed |
title | Relationship between coral distributions and physical variables in Amitori Bay, Iriomote Island, Japan |
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