New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera

Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common...
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Autor*in:	Kharlamenko, Vladimir I. [verfasserIn] Svetashev, Vasily I. [verfasserIn] Tarasova, Tatyana S. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Deep-sea Foraminifera Polyunsaturated fatty acids Non-methylene interrupted diunsaturated FA New and rare fatty acids and

Übergeordnetes Werk:	Enthalten in: Lipids - Hoboken, NJ : Wiley, 1966, 52(2017), 4 vom: 16. Feb., Seite 345-352
Übergeordnetes Werk:	volume:52 ; year:2017 ; number:4 ; day:16 ; month:02 ; pages:345-352

Links:	Volltext

DOI / URN:	10.1007/s11745-017-4237-2

Katalog-ID:	SPR022185151

Internformat


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100	1		\|a Kharlamenko, Vladimir I. \|e verfasserin \|4 aut
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520			\|a Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed.
650		4	\|a Deep-sea Foraminifera \|7 (dpeaa)DE-He213
650		4	\|a Polyunsaturated fatty acids \|7 (dpeaa)DE-He213
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650		4	\|a New and rare fatty acids \|7 (dpeaa)DE-He213
650		4	\|a and \|7 (dpeaa)DE-He213
700	1		\|a Svetashev, Vasily I. \|e verfasserin \|4 aut
700	1		\|a Tarasova, Tatyana S. \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Lipids \|d Hoboken, NJ : Wiley, 1966 \|g 52(2017), 4 vom: 16. Feb., Seite 345-352 \|w (DE-627)324743122 \|w (DE-600)2030265-4 \|x 1558-9307 \|7 nnns
773	1	8	\|g volume:52 \|g year:2017 \|g number:4 \|g day:16 \|g month:02 \|g pages:345-352
856	4	0	\|u https://dx.doi.org/10.1007/s11745-017-4237-2 \|z lizenzpflichtig \|3 Volltext
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912			\|a GBV_ILN_20
912			\|a GBV_ILN_22
912			\|a GBV_ILN_23
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_32
912			\|a GBV_ILN_39
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_101
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_120
912			\|a GBV_ILN_138
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
912			\|a GBV_ILN_171
912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_266
912			\|a GBV_ILN_285
912			\|a GBV_ILN_293
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_636
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2001
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
912			\|a GBV_ILN_2007
912			\|a GBV_ILN_2008
912			\|a GBV_ILN_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2018
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2031
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2037
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2039
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2055
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2057
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2070
912			\|a GBV_ILN_2086
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2108
912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2116
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2119
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2144
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2188
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2232
912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2470
912			\|a GBV_ILN_2472
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_2548
912			\|a GBV_ILN_4012
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4046
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4246
912			\|a GBV_ILN_4249
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4306
912			\|a GBV_ILN_4307
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4336
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
912			\|a GBV_ILN_4700
936	b	k	\|a 35.78 \|q ASE
951			\|a AR
952			\|d 52 \|j 2017 \|e 4 \|b 16 \|c 02 \|h 345-352

Indexfelder

author_variant	v i k vi vik v i s vi vis t s t ts tst
matchkey_str	article:15589307:2017----::eadnomnataisniisfep
hierarchy_sort_str	2017
bklnumber	35.78
publishDate	2017
allfields	10.1007/s11745-017-4237-2 doi (DE-627)SPR022185151 (SPR)s11745-017-4237-2-e DE-627 ger DE-627 rakwb eng 540 ASE 35.78 bkl Kharlamenko, Vladimir I. verfasserin aut New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed. Deep-sea Foraminifera (dpeaa)DE-He213 Polyunsaturated fatty acids (dpeaa)DE-He213 Non-methylene interrupted diunsaturated FA (dpeaa)DE-He213 New and rare fatty acids (dpeaa)DE-He213 and (dpeaa)DE-He213 Svetashev, Vasily I. verfasserin aut Tarasova, Tatyana S. verfasserin aut Enthalten in Lipids Hoboken, NJ : Wiley, 1966 52(2017), 4 vom: 16. Feb., Seite 345-352 (DE-627)324743122 (DE-600)2030265-4 1558-9307 nnns volume:52 year:2017 number:4 day:16 month:02 pages:345-352 https://dx.doi.org/10.1007/s11745-017-4237-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_101 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_266 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_2018 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_2056 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_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_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 35.78 ASE AR 52 2017 4 16 02 345-352
spelling	10.1007/s11745-017-4237-2 doi (DE-627)SPR022185151 (SPR)s11745-017-4237-2-e DE-627 ger DE-627 rakwb eng 540 ASE 35.78 bkl Kharlamenko, Vladimir I. verfasserin aut New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed. Deep-sea Foraminifera (dpeaa)DE-He213 Polyunsaturated fatty acids (dpeaa)DE-He213 Non-methylene interrupted diunsaturated FA (dpeaa)DE-He213 New and rare fatty acids (dpeaa)DE-He213 and (dpeaa)DE-He213 Svetashev, Vasily I. verfasserin aut Tarasova, Tatyana S. verfasserin aut Enthalten in Lipids Hoboken, NJ : Wiley, 1966 52(2017), 4 vom: 16. Feb., Seite 345-352 (DE-627)324743122 (DE-600)2030265-4 1558-9307 nnns volume:52 year:2017 number:4 day:16 month:02 pages:345-352 https://dx.doi.org/10.1007/s11745-017-4237-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_101 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_266 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_2018 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_2056 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_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_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 35.78 ASE AR 52 2017 4 16 02 345-352
allfields_unstemmed	10.1007/s11745-017-4237-2 doi (DE-627)SPR022185151 (SPR)s11745-017-4237-2-e DE-627 ger DE-627 rakwb eng 540 ASE 35.78 bkl Kharlamenko, Vladimir I. verfasserin aut New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed. Deep-sea Foraminifera (dpeaa)DE-He213 Polyunsaturated fatty acids (dpeaa)DE-He213 Non-methylene interrupted diunsaturated FA (dpeaa)DE-He213 New and rare fatty acids (dpeaa)DE-He213 and (dpeaa)DE-He213 Svetashev, Vasily I. verfasserin aut Tarasova, Tatyana S. verfasserin aut Enthalten in Lipids Hoboken, NJ : Wiley, 1966 52(2017), 4 vom: 16. Feb., Seite 345-352 (DE-627)324743122 (DE-600)2030265-4 1558-9307 nnns volume:52 year:2017 number:4 day:16 month:02 pages:345-352 https://dx.doi.org/10.1007/s11745-017-4237-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_101 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_266 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_2018 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_2056 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_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_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 35.78 ASE AR 52 2017 4 16 02 345-352
allfieldsGer	10.1007/s11745-017-4237-2 doi (DE-627)SPR022185151 (SPR)s11745-017-4237-2-e DE-627 ger DE-627 rakwb eng 540 ASE 35.78 bkl Kharlamenko, Vladimir I. verfasserin aut New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed. Deep-sea Foraminifera (dpeaa)DE-He213 Polyunsaturated fatty acids (dpeaa)DE-He213 Non-methylene interrupted diunsaturated FA (dpeaa)DE-He213 New and rare fatty acids (dpeaa)DE-He213 and (dpeaa)DE-He213 Svetashev, Vasily I. verfasserin aut Tarasova, Tatyana S. verfasserin aut Enthalten in Lipids Hoboken, NJ : Wiley, 1966 52(2017), 4 vom: 16. Feb., Seite 345-352 (DE-627)324743122 (DE-600)2030265-4 1558-9307 nnns volume:52 year:2017 number:4 day:16 month:02 pages:345-352 https://dx.doi.org/10.1007/s11745-017-4237-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_101 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_266 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_2018 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_2056 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_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_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 35.78 ASE AR 52 2017 4 16 02 345-352
allfieldsSound	10.1007/s11745-017-4237-2 doi (DE-627)SPR022185151 (SPR)s11745-017-4237-2-e DE-627 ger DE-627 rakwb eng 540 ASE 35.78 bkl Kharlamenko, Vladimir I. verfasserin aut New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed. Deep-sea Foraminifera (dpeaa)DE-He213 Polyunsaturated fatty acids (dpeaa)DE-He213 Non-methylene interrupted diunsaturated FA (dpeaa)DE-He213 New and rare fatty acids (dpeaa)DE-He213 and (dpeaa)DE-He213 Svetashev, Vasily I. verfasserin aut Tarasova, Tatyana S. verfasserin aut Enthalten in Lipids Hoboken, NJ : Wiley, 1966 52(2017), 4 vom: 16. Feb., Seite 345-352 (DE-627)324743122 (DE-600)2030265-4 1558-9307 nnns volume:52 year:2017 number:4 day:16 month:02 pages:345-352 https://dx.doi.org/10.1007/s11745-017-4237-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA 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_101 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_266 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_2018 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_2056 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_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_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 35.78 ASE AR 52 2017 4 16 02 345-352
language	English
source	Enthalten in Lipids 52(2017), 4 vom: 16. Feb., Seite 345-352 volume:52 year:2017 number:4 day:16 month:02 pages:345-352
sourceStr	Enthalten in Lipids 52(2017), 4 vom: 16. Feb., Seite 345-352 volume:52 year:2017 number:4 day:16 month:02 pages:345-352
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Deep-sea Foraminifera Polyunsaturated fatty acids Non-methylene interrupted diunsaturated FA New and rare fatty acids and
dewey-raw	540
isfreeaccess_bool	false
container_title	Lipids
authorswithroles_txt_mv	Kharlamenko, Vladimir I. @@aut@@ Svetashev, Vasily I. @@aut@@ Tarasova, Tatyana S. @@aut@@
publishDateDaySort_date	2017-02-16T00:00:00Z
hierarchy_top_id	324743122
dewey-sort	3540
id	SPR022185151
language_de	englisch
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author	Kharlamenko, Vladimir I.
spellingShingle	Kharlamenko, Vladimir I. ddc 540 bkl 35.78 misc Deep-sea Foraminifera misc Polyunsaturated fatty acids misc Non-methylene interrupted diunsaturated FA misc New and rare fatty acids misc and New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera
authorStr	Kharlamenko, Vladimir I.
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topic_title	540 ASE 35.78 bkl New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera Deep-sea Foraminifera (dpeaa)DE-He213 Polyunsaturated fatty acids (dpeaa)DE-He213 Non-methylene interrupted diunsaturated FA (dpeaa)DE-He213 New and rare fatty acids (dpeaa)DE-He213 and (dpeaa)DE-He213
topic	ddc 540 bkl 35.78 misc Deep-sea Foraminifera misc Polyunsaturated fatty acids misc Non-methylene interrupted diunsaturated FA misc New and rare fatty acids misc and
topic_unstemmed	ddc 540 bkl 35.78 misc Deep-sea Foraminifera misc Polyunsaturated fatty acids misc Non-methylene interrupted diunsaturated FA misc New and rare fatty acids misc and
topic_browse	ddc 540 bkl 35.78 misc Deep-sea Foraminifera misc Polyunsaturated fatty acids misc Non-methylene interrupted diunsaturated FA misc New and rare fatty acids misc and
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title	New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera
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title_full	New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera
author_sort	Kharlamenko, Vladimir I.
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title_sort	new and uncommon fatty acids in lipids of deep-sea foraminifera
title_auth	New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera
abstract	Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed.
abstractGer	Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed.
abstract_unstemmed	Abstract Fatty acids (FA) of agglutinating foraminifera of two genera, Bathysiphon and Rhabdammina, collected from a depth of 3307–3377 m in the Kuril Basin, Sea of Okhotsk, and adjacent deep-sea waters of the Pacific Ocean, were analyzed. In lipids of two Bathysiphon species, in addition to common FA typical for marine organisms, the uncommon ∆4 and ∆7 monoenoic acids and ∆4,7-dienoic acid were found in noticeable amounts. FA of two Rhabdammina species included also such uncommon acids as ∆5,8,11,14–21:4, ∆5,8,11,14–22:4, and ∆5,8,11,14–23:4, which are homologues to arachidonic acid. High levels of cis-vaccenic and arachidonic acids were typical for lipids of all the studied species. At the same time, we observed a substantial difference in FA composition between members of these two genera. Using GC and GC–MS of FAME, pyrrolidide and DMOX derivatives, the structures of 10 new FA were confirmed: ∆4-i-16:1 (1.1–0.6%), ∆7-i-21:1 (0.4%), ∆7-ai-21:1 (0.3–0.8%), ∆4,11–18:2 (0.3–0.9%), ∆4,7–20:2 (8.8%), ∆7,12–20:2 (0.4–0.6%), ∆4,7–21:2 (0.6%), ∆7,12–22:2 (6.4–2.1%); ∆5,8,11,14–22:4 (1.2–2.0%), and ∆5,8,11,14–23:4 (1.7–2.3%). The origin of the new FA and the role of foraminifera FA in deep-sea communities are discussed.
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container_issue	4
title_short	New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera
url	https://dx.doi.org/10.1007/s11745-017-4237-2
remote_bool	true
author2	Svetashev, Vasily I. Tarasova, Tatyana S.
author2Str	Svetashev, Vasily I. Tarasova, Tatyana S.
ppnlink	324743122
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isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1007/s11745-017-4237-2
up_date	2024-07-04T02:10:26.544Z
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New and Uncommon Fatty Acids in Lipids of Deep-Sea Foraminifera

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