Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?

Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be...
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Autor*in:	Pronin, Eugeniusz [verfasserIn] Banaś, Krzysztof Chmara, Rafał Ronowski, Rafał Merdalski, Marek Santoni, Anne-Lise Mathieu, Olivier

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	C N Macrophytes Charophytes Organic matter Water chemistry

Anmerkung:	© The Author(s) 2023

Übergeordnetes Werk:	Enthalten in: Aquatic sciences - Basel : Springer, 1920, 85(2023), 3 vom: 28. Mai
Übergeordnetes Werk:	volume:85 ; year:2023 ; number:3 ; day:28 ; month:05

Links:	Volltext

DOI / URN:	10.1007/s00027-023-00976-6

Katalog-ID:	SPR051678543

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100	1		\|a Pronin, Eugeniusz \|e verfasserin \|0 (orcid)0000-0002-4641-452X \|4 aut
245	1	0	\|a Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?
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520			\|a Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water.
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700	1		\|a Banaś, Krzysztof \|0 (orcid)0000-0002-2131-8400 \|4 aut
700	1		\|a Chmara, Rafał \|0 (orcid)0000-0002-9267-5085 \|4 aut
700	1		\|a Ronowski, Rafał \|0 (orcid)0000-0002-5638-7131 \|4 aut
700	1		\|a Merdalski, Marek \|0 (orcid)0000-0003-2117-4889 \|4 aut
700	1		\|a Santoni, Anne-Lise \|0 (orcid)0000-0002-1404-6187 \|4 aut
700	1		\|a Mathieu, Olivier \|0 (orcid)0000-0002-6387-6996 \|4 aut
773	0	8	\|i Enthalten in \|t Aquatic sciences \|d Basel : Springer, 1920 \|g 85(2023), 3 vom: 28. Mai \|w (DE-627)265506670 \|w (DE-600)1464021-1 \|x 1420-9055 \|7 nnns
773	1	8	\|g volume:85 \|g year:2023 \|g number:3 \|g day:28 \|g month:05
856	4	0	\|u https://dx.doi.org/10.1007/s00027-023-00976-6 \|z kostenfrei \|3 Volltext
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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_250
912			\|a GBV_ILN_267
912			\|a GBV_ILN_281
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_2009
912			\|a GBV_ILN_2010
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
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912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2026
912			\|a GBV_ILN_2027
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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_2088
912			\|a GBV_ILN_2093
912			\|a GBV_ILN_2106
912			\|a GBV_ILN_2107
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912			\|a GBV_ILN_2110
912			\|a GBV_ILN_2111
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912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
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Indexfelder

author_variant	e p ep k b kb r c rc r r rr m m mm a l s als o m om
matchkey_str	article:14209055:2023----::otbeabnnntoeiooeausfielfeiidfebten
hierarchy_sort_str	2023
publishDate	2023
allfields	10.1007/s00027-023-00976-6 doi (DE-627)SPR051678543 (SPR)s00027-023-00976-6-e DE-627 ger DE-627 rakwb eng Pronin, Eugeniusz verfasserin (orcid)0000-0002-4641-452X aut Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes? 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. C (dpeaa)DE-He213 N (dpeaa)DE-He213 Macrophytes (dpeaa)DE-He213 Charophytes (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Water chemistry (dpeaa)DE-He213 Banaś, Krzysztof (orcid)0000-0002-2131-8400 aut Chmara, Rafał (orcid)0000-0002-9267-5085 aut Ronowski, Rafał (orcid)0000-0002-5638-7131 aut Merdalski, Marek (orcid)0000-0003-2117-4889 aut Santoni, Anne-Lise (orcid)0000-0002-1404-6187 aut Mathieu, Olivier (orcid)0000-0002-6387-6996 aut Enthalten in Aquatic sciences Basel : Springer, 1920 85(2023), 3 vom: 28. Mai (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:85 year:2023 number:3 day:28 month:05 https://dx.doi.org/10.1007/s00027-023-00976-6 kostenfrei 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_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_267 GBV_ILN_281 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2023 3 28 05
spelling	10.1007/s00027-023-00976-6 doi (DE-627)SPR051678543 (SPR)s00027-023-00976-6-e DE-627 ger DE-627 rakwb eng Pronin, Eugeniusz verfasserin (orcid)0000-0002-4641-452X aut Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes? 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. C (dpeaa)DE-He213 N (dpeaa)DE-He213 Macrophytes (dpeaa)DE-He213 Charophytes (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Water chemistry (dpeaa)DE-He213 Banaś, Krzysztof (orcid)0000-0002-2131-8400 aut Chmara, Rafał (orcid)0000-0002-9267-5085 aut Ronowski, Rafał (orcid)0000-0002-5638-7131 aut Merdalski, Marek (orcid)0000-0003-2117-4889 aut Santoni, Anne-Lise (orcid)0000-0002-1404-6187 aut Mathieu, Olivier (orcid)0000-0002-6387-6996 aut Enthalten in Aquatic sciences Basel : Springer, 1920 85(2023), 3 vom: 28. Mai (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:85 year:2023 number:3 day:28 month:05 https://dx.doi.org/10.1007/s00027-023-00976-6 kostenfrei 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_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_267 GBV_ILN_281 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2023 3 28 05
allfields_unstemmed	10.1007/s00027-023-00976-6 doi (DE-627)SPR051678543 (SPR)s00027-023-00976-6-e DE-627 ger DE-627 rakwb eng Pronin, Eugeniusz verfasserin (orcid)0000-0002-4641-452X aut Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes? 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. C (dpeaa)DE-He213 N (dpeaa)DE-He213 Macrophytes (dpeaa)DE-He213 Charophytes (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Water chemistry (dpeaa)DE-He213 Banaś, Krzysztof (orcid)0000-0002-2131-8400 aut Chmara, Rafał (orcid)0000-0002-9267-5085 aut Ronowski, Rafał (orcid)0000-0002-5638-7131 aut Merdalski, Marek (orcid)0000-0003-2117-4889 aut Santoni, Anne-Lise (orcid)0000-0002-1404-6187 aut Mathieu, Olivier (orcid)0000-0002-6387-6996 aut Enthalten in Aquatic sciences Basel : Springer, 1920 85(2023), 3 vom: 28. Mai (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:85 year:2023 number:3 day:28 month:05 https://dx.doi.org/10.1007/s00027-023-00976-6 kostenfrei 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_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_267 GBV_ILN_281 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2023 3 28 05
allfieldsGer	10.1007/s00027-023-00976-6 doi (DE-627)SPR051678543 (SPR)s00027-023-00976-6-e DE-627 ger DE-627 rakwb eng Pronin, Eugeniusz verfasserin (orcid)0000-0002-4641-452X aut Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes? 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. C (dpeaa)DE-He213 N (dpeaa)DE-He213 Macrophytes (dpeaa)DE-He213 Charophytes (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Water chemistry (dpeaa)DE-He213 Banaś, Krzysztof (orcid)0000-0002-2131-8400 aut Chmara, Rafał (orcid)0000-0002-9267-5085 aut Ronowski, Rafał (orcid)0000-0002-5638-7131 aut Merdalski, Marek (orcid)0000-0003-2117-4889 aut Santoni, Anne-Lise (orcid)0000-0002-1404-6187 aut Mathieu, Olivier (orcid)0000-0002-6387-6996 aut Enthalten in Aquatic sciences Basel : Springer, 1920 85(2023), 3 vom: 28. Mai (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:85 year:2023 number:3 day:28 month:05 https://dx.doi.org/10.1007/s00027-023-00976-6 kostenfrei 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_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_267 GBV_ILN_281 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2023 3 28 05
allfieldsSound	10.1007/s00027-023-00976-6 doi (DE-627)SPR051678543 (SPR)s00027-023-00976-6-e DE-627 ger DE-627 rakwb eng Pronin, Eugeniusz verfasserin (orcid)0000-0002-4641-452X aut Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes? 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. C (dpeaa)DE-He213 N (dpeaa)DE-He213 Macrophytes (dpeaa)DE-He213 Charophytes (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Water chemistry (dpeaa)DE-He213 Banaś, Krzysztof (orcid)0000-0002-2131-8400 aut Chmara, Rafał (orcid)0000-0002-9267-5085 aut Ronowski, Rafał (orcid)0000-0002-5638-7131 aut Merdalski, Marek (orcid)0000-0003-2117-4889 aut Santoni, Anne-Lise (orcid)0000-0002-1404-6187 aut Mathieu, Olivier (orcid)0000-0002-6387-6996 aut Enthalten in Aquatic sciences Basel : Springer, 1920 85(2023), 3 vom: 28. Mai (DE-627)265506670 (DE-600)1464021-1 1420-9055 nnns volume:85 year:2023 number:3 day:28 month:05 https://dx.doi.org/10.1007/s00027-023-00976-6 kostenfrei 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_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_267 GBV_ILN_281 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_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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 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_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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2023 3 28 05
language	English
source	Enthalten in Aquatic sciences 85(2023), 3 vom: 28. Mai volume:85 year:2023 number:3 day:28 month:05
sourceStr	Enthalten in Aquatic sciences 85(2023), 3 vom: 28. Mai volume:85 year:2023 number:3 day:28 month:05
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	C N Macrophytes Charophytes Organic matter Water chemistry
isfreeaccess_bool	true
container_title	Aquatic sciences
authorswithroles_txt_mv	Pronin, Eugeniusz @@aut@@ Banaś, Krzysztof @@aut@@ Chmara, Rafał @@aut@@ Ronowski, Rafał @@aut@@ Merdalski, Marek @@aut@@ Santoni, Anne-Lise @@aut@@ Mathieu, Olivier @@aut@@
publishDateDaySort_date	2023-05-28T00:00:00Z
hierarchy_top_id	265506670
id	SPR051678543
language_de	englisch
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author	Pronin, Eugeniusz
spellingShingle	Pronin, Eugeniusz misc C misc N misc Macrophytes misc Charophytes misc Organic matter misc Water chemistry Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?
authorStr	Pronin, Eugeniusz
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topic_title	Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes? C (dpeaa)DE-He213 N (dpeaa)DE-He213 Macrophytes (dpeaa)DE-He213 Charophytes (dpeaa)DE-He213 Organic matter (dpeaa)DE-He213 Water chemistry (dpeaa)DE-He213
topic	misc C misc N misc Macrophytes misc Charophytes misc Organic matter misc Water chemistry
topic_unstemmed	misc C misc N misc Macrophytes misc Charophytes misc Organic matter misc Water chemistry
topic_browse	misc C misc N misc Macrophytes misc Charophytes misc Organic matter misc Water chemistry
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
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title	Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?
ctrlnum	(DE-627)SPR051678543 (SPR)s00027-023-00976-6-e
title_full	Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?
author_sort	Pronin, Eugeniusz
journal	Aquatic sciences
journalStr	Aquatic sciences
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author_browse	Pronin, Eugeniusz Banaś, Krzysztof Chmara, Rafał Ronowski, Rafał Merdalski, Marek Santoni, Anne-Lise Mathieu, Olivier
container_volume	85
format_se	Elektronische Aufsätze
author-letter	Pronin, Eugeniusz
doi_str_mv	10.1007/s00027-023-00976-6
normlink	(ORCID)0000-0002-4641-452X (ORCID)0000-0002-2131-8400 (ORCID)0000-0002-9267-5085 (ORCID)0000-0002-5638-7131 (ORCID)0000-0003-2117-4889 (ORCID)0000-0002-1404-6187 (ORCID)0000-0002-6387-6996
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title_sort	do stable carbon and nitrogen isotope values of nitella flexilis differ between softwater and hardwater lakes?
title_auth	Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?
abstract	Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. © The Author(s) 2023
abstractGer	Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. © The Author(s) 2023
abstract_unstemmed	Abstract The composition of stable carbon and nitrogen isotopes (δ13C and δ15N) is widely used for tracking the origin of organic matter (OM) present in lacustrine sediments. These isotopes also define the evolution of OM in food web loops. Charophyte species Nitella flexilis C. Agardh, 1824 can be found in different aquatic environments where it contributes significantly to sediment formation and influences biota function. Therefore, it is crucial to study more about δ13C and δ15N in different lake types. Here, we present the results of the first comprehensive study of N. flexilis δ13C and δ15N, which add to the knowledge of the C and N isotope records of charophytes. We obtained the δ13C and δ15N records of N. flexilis OM from hardwater and softwater lakes and checked for differences between these records. We also analyzed the differences in physical and chemical parameters. Finally, we compared the δ13C and δ15N records with physical and chemical parameters to identify the variables that have the highest influence on N. flexilis δ13C and δ15N values. Our study showed that both δ13C and δ15N did not differ significantly in the two types of lakes, although the lakes had significant differences in several physical and chemical parameters (pH, $ Ca^{2+} $, dissolved inorganic carbon, total phosphorus, conductivity). However, we observed that δ13C values were influenced by light conditions (photosynthetic active radiation, depth, dissolved OM), while δ15N values were influenced by the total nitrogen concentration in water. © The Author(s) 2023
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container_issue	3
title_short	Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?
url	https://dx.doi.org/10.1007/s00027-023-00976-6
remote_bool	true
author2	Banaś, Krzysztof Chmara, Rafał Ronowski, Rafał Merdalski, Marek Santoni, Anne-Lise Mathieu, Olivier
author2Str	Banaś, Krzysztof Chmara, Rafał Ronowski, Rafał Merdalski, Marek Santoni, Anne-Lise Mathieu, Olivier
ppnlink	265506670
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doi_str	10.1007/s00027-023-00976-6
up_date	2024-07-03T23:12:41.941Z
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Do stable carbon and nitrogen isotope values of Nitella flexilis differ between softwater and hardwater lakes?

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