Distribution of benthic foraminifera along the Iranian coast
Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed...
Ausführliche Beschreibung
Autor*in: |
Amao, Abduljamiu O. [verfasserIn] Kaminski, Michael A. [verfasserIn] Asgharian Rostami, Masoud [verfasserIn] Gharaie, Mohamad Hosein Mahmudy [verfasserIn] Lak, Razyeh [verfasserIn] Frontalini, Fabrizio [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2018 |
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Übergeordnetes Werk: |
Enthalten in: Marine biodiversity - Berlin : Springer, 2009, 49(2018), 2 vom: 09. Apr., Seite 933-946 |
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Übergeordnetes Werk: |
volume:49 ; year:2018 ; number:2 ; day:09 ; month:04 ; pages:933-946 |
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DOI / URN: |
10.1007/s12526-018-0879-4 |
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Katalog-ID: |
SPR02603932X |
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520 | |a Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. | ||
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650 | 4 | |a Persian Gulf |7 (dpeaa)DE-He213 | |
650 | 4 | |a Benthic foraminifera |7 (dpeaa)DE-He213 | |
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650 | 4 | |a Iranian coast |7 (dpeaa)DE-He213 | |
700 | 1 | |a Kaminski, Michael A. |e verfasserin |4 aut | |
700 | 1 | |a Asgharian Rostami, Masoud |e verfasserin |4 aut | |
700 | 1 | |a Gharaie, Mohamad Hosein Mahmudy |e verfasserin |4 aut | |
700 | 1 | |a Lak, Razyeh |e verfasserin |4 aut | |
700 | 1 | |a Frontalini, Fabrizio |e verfasserin |4 aut | |
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10.1007/s12526-018-0879-4 doi (DE-627)SPR02603932X (SPR)s12526-018-0879-4-e DE-627 ger DE-627 rakwb eng 550 ASE Amao, Abduljamiu O. verfasserin aut Distribution of benthic foraminifera along the Iranian coast 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. The Gulf (dpeaa)DE-He213 Arabian Gulf (dpeaa)DE-He213 Persian Gulf (dpeaa)DE-He213 Benthic foraminifera (dpeaa)DE-He213 Diversity (dpeaa)DE-He213 Iranian coast (dpeaa)DE-He213 Kaminski, Michael A. verfasserin aut Asgharian Rostami, Masoud verfasserin aut Gharaie, Mohamad Hosein Mahmudy verfasserin aut Lak, Razyeh verfasserin aut Frontalini, Fabrizio verfasserin aut Enthalten in Marine biodiversity Berlin : Springer, 2009 49(2018), 2 vom: 09. Apr., Seite 933-946 (DE-627)599671955 (DE-600)2493558-X 1867-1624 nnns volume:49 year:2018 number:2 day:09 month:04 pages:933-946 https://dx.doi.org/10.1007/s12526-018-0879-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 49 2018 2 09 04 933-946 |
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10.1007/s12526-018-0879-4 doi (DE-627)SPR02603932X (SPR)s12526-018-0879-4-e DE-627 ger DE-627 rakwb eng 550 ASE Amao, Abduljamiu O. verfasserin aut Distribution of benthic foraminifera along the Iranian coast 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. The Gulf (dpeaa)DE-He213 Arabian Gulf (dpeaa)DE-He213 Persian Gulf (dpeaa)DE-He213 Benthic foraminifera (dpeaa)DE-He213 Diversity (dpeaa)DE-He213 Iranian coast (dpeaa)DE-He213 Kaminski, Michael A. verfasserin aut Asgharian Rostami, Masoud verfasserin aut Gharaie, Mohamad Hosein Mahmudy verfasserin aut Lak, Razyeh verfasserin aut Frontalini, Fabrizio verfasserin aut Enthalten in Marine biodiversity Berlin : Springer, 2009 49(2018), 2 vom: 09. Apr., Seite 933-946 (DE-627)599671955 (DE-600)2493558-X 1867-1624 nnns volume:49 year:2018 number:2 day:09 month:04 pages:933-946 https://dx.doi.org/10.1007/s12526-018-0879-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 49 2018 2 09 04 933-946 |
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10.1007/s12526-018-0879-4 doi (DE-627)SPR02603932X (SPR)s12526-018-0879-4-e DE-627 ger DE-627 rakwb eng 550 ASE Amao, Abduljamiu O. verfasserin aut Distribution of benthic foraminifera along the Iranian coast 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. The Gulf (dpeaa)DE-He213 Arabian Gulf (dpeaa)DE-He213 Persian Gulf (dpeaa)DE-He213 Benthic foraminifera (dpeaa)DE-He213 Diversity (dpeaa)DE-He213 Iranian coast (dpeaa)DE-He213 Kaminski, Michael A. verfasserin aut Asgharian Rostami, Masoud verfasserin aut Gharaie, Mohamad Hosein Mahmudy verfasserin aut Lak, Razyeh verfasserin aut Frontalini, Fabrizio verfasserin aut Enthalten in Marine biodiversity Berlin : Springer, 2009 49(2018), 2 vom: 09. Apr., Seite 933-946 (DE-627)599671955 (DE-600)2493558-X 1867-1624 nnns volume:49 year:2018 number:2 day:09 month:04 pages:933-946 https://dx.doi.org/10.1007/s12526-018-0879-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 49 2018 2 09 04 933-946 |
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10.1007/s12526-018-0879-4 doi (DE-627)SPR02603932X (SPR)s12526-018-0879-4-e DE-627 ger DE-627 rakwb eng 550 ASE Amao, Abduljamiu O. verfasserin aut Distribution of benthic foraminifera along the Iranian coast 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. The Gulf (dpeaa)DE-He213 Arabian Gulf (dpeaa)DE-He213 Persian Gulf (dpeaa)DE-He213 Benthic foraminifera (dpeaa)DE-He213 Diversity (dpeaa)DE-He213 Iranian coast (dpeaa)DE-He213 Kaminski, Michael A. verfasserin aut Asgharian Rostami, Masoud verfasserin aut Gharaie, Mohamad Hosein Mahmudy verfasserin aut Lak, Razyeh verfasserin aut Frontalini, Fabrizio verfasserin aut Enthalten in Marine biodiversity Berlin : Springer, 2009 49(2018), 2 vom: 09. Apr., Seite 933-946 (DE-627)599671955 (DE-600)2493558-X 1867-1624 nnns volume:49 year:2018 number:2 day:09 month:04 pages:933-946 https://dx.doi.org/10.1007/s12526-018-0879-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 49 2018 2 09 04 933-946 |
allfieldsSound |
10.1007/s12526-018-0879-4 doi (DE-627)SPR02603932X (SPR)s12526-018-0879-4-e DE-627 ger DE-627 rakwb eng 550 ASE Amao, Abduljamiu O. verfasserin aut Distribution of benthic foraminifera along the Iranian coast 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. The Gulf (dpeaa)DE-He213 Arabian Gulf (dpeaa)DE-He213 Persian Gulf (dpeaa)DE-He213 Benthic foraminifera (dpeaa)DE-He213 Diversity (dpeaa)DE-He213 Iranian coast (dpeaa)DE-He213 Kaminski, Michael A. verfasserin aut Asgharian Rostami, Masoud verfasserin aut Gharaie, Mohamad Hosein Mahmudy verfasserin aut Lak, Razyeh verfasserin aut Frontalini, Fabrizio verfasserin aut Enthalten in Marine biodiversity Berlin : Springer, 2009 49(2018), 2 vom: 09. Apr., Seite 933-946 (DE-627)599671955 (DE-600)2493558-X 1867-1624 nnns volume:49 year:2018 number:2 day:09 month:04 pages:933-946 https://dx.doi.org/10.1007/s12526-018-0879-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 49 2018 2 09 04 933-946 |
language |
English |
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Enthalten in Marine biodiversity 49(2018), 2 vom: 09. Apr., Seite 933-946 volume:49 year:2018 number:2 day:09 month:04 pages:933-946 |
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Enthalten in Marine biodiversity 49(2018), 2 vom: 09. Apr., Seite 933-946 volume:49 year:2018 number:2 day:09 month:04 pages:933-946 |
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The Gulf Arabian Gulf Persian Gulf Benthic foraminifera Diversity Iranian coast |
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Marine biodiversity |
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Amao, Abduljamiu O. @@aut@@ Kaminski, Michael A. @@aut@@ Asgharian Rostami, Masoud @@aut@@ Gharaie, Mohamad Hosein Mahmudy @@aut@@ Lak, Razyeh @@aut@@ Frontalini, Fabrizio @@aut@@ |
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2018-04-09T00:00:00Z |
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The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. 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|
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Amao, Abduljamiu O. |
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Amao, Abduljamiu O. ddc 550 misc The Gulf misc Arabian Gulf misc Persian Gulf misc Benthic foraminifera misc Diversity misc Iranian coast Distribution of benthic foraminifera along the Iranian coast |
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550 ASE Distribution of benthic foraminifera along the Iranian coast The Gulf (dpeaa)DE-He213 Arabian Gulf (dpeaa)DE-He213 Persian Gulf (dpeaa)DE-He213 Benthic foraminifera (dpeaa)DE-He213 Diversity (dpeaa)DE-He213 Iranian coast (dpeaa)DE-He213 |
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ddc 550 misc The Gulf misc Arabian Gulf misc Persian Gulf misc Benthic foraminifera misc Diversity misc Iranian coast |
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ddc 550 misc The Gulf misc Arabian Gulf misc Persian Gulf misc Benthic foraminifera misc Diversity misc Iranian coast |
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Distribution of benthic foraminifera along the Iranian coast |
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Distribution of benthic foraminifera along the Iranian coast |
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Amao, Abduljamiu O. |
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Marine biodiversity |
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Marine biodiversity |
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Amao, Abduljamiu O. Kaminski, Michael A. Asgharian Rostami, Masoud Gharaie, Mohamad Hosein Mahmudy Lak, Razyeh Frontalini, Fabrizio |
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Amao, Abduljamiu O. |
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distribution of benthic foraminifera along the iranian coast |
title_auth |
Distribution of benthic foraminifera along the Iranian coast |
abstract |
Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. |
abstractGer |
Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. |
abstract_unstemmed |
Abstract This study focuses on the distribution of benthic foraminifera along the Iranian coast of the Gulf, extending over 1000 km from the northeast close to Shatt Al-Arab/Arvand Rud to the southeast near the Strait of Hormuz where it connects to the Indian Ocean. The Gulf is a naturally stressed environment due to extremes of salinity and temperature and anthropogenically affected by rapid urbanization, maritime transport, desalination plants, and oil platforms. Historical records and distributional studies have commonly underestimated the benthic foraminiferal diversity in the Gulf. Thirty-two samples collected from depths between 20 and 45 m were analyzed for total (unstained) foraminiferal assemblages. A total of 221 benthic foraminiferal species and subspecies belonging to 69 genera, 34 families, and 6 orders were recognized. The assemblages are dominated by hyaline taxa (49%) and porcelaneous foraminifera (36%), while agglutinated foraminifera represent only a minor part (15%). The ten most abundant species are Nonion sp. 1 (5.8%), Quinqueloculina sp. 1 (4.7%), Asterorotalia dentata (4.2%), Bolivina cf. B. persiensis (3.9%), Asterorotalia sp. 3 (3.5%), Rotalinoides gaimardi (3.4%), Ammonia sp. 1 (3.3%), Quinqueloculina sp. 8 (3.3%), Bolivina cf. B. striatula (3.0%), and Nonion sp. 2 (2.8%). We speculate that increase of finer sediments (mud), availability of nutrients, and the presence of oxygen are factors controlling the diversity and distribution of benthic foraminifera. The current thermal regime in the Gulf has been cited as a model for the tropical ocean in 2090–2099. In light of it, foraminiferal assemblage structure, composition, and distribution may provide an insight into the nature of biotic response to future climate change in the Gulf region under conditions of global warming and a baseline for future comparison within and beyond the Gulf. This study also updates the knowledge on the types and distributions of benthic foraminiferal groups in this poorly known area. |
collection_details |
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container_issue |
2 |
title_short |
Distribution of benthic foraminifera along the Iranian coast |
url |
https://dx.doi.org/10.1007/s12526-018-0879-4 |
remote_bool |
true |
author2 |
Kaminski, Michael A. Asgharian Rostami, Masoud Gharaie, Mohamad Hosein Mahmudy Lak, Razyeh Frontalini, Fabrizio |
author2Str |
Kaminski, Michael A. Asgharian Rostami, Masoud Gharaie, Mohamad Hosein Mahmudy Lak, Razyeh Frontalini, Fabrizio |
ppnlink |
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mediatype_str_mv |
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isOA_txt |
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hochschulschrift_bool |
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doi_str |
10.1007/s12526-018-0879-4 |
up_date |
2024-07-03T18:30:48.841Z |
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score |
7.3986673 |