Study on chemical hydrography, chlorophyll-
A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton prod...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Pei, Shaofeng [verfasserIn] Laws, Edward A. [verfasserIn] Zhang, Haibo [verfasserIn] Ye, Siyuan [verfasserIn] Kemper, Marc T. [verfasserIn] Yuan, Hongming [verfasserIn] Xu, Gang [verfasserIn] Yang, Shixiong [verfasserIn] Liu, Haiyue [verfasserIn] Zhu, Yaxuan [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Estuarine, coastal and shelf science - London : Academic Press, 1981, 202, Seite 103-113 |
|---|---|
| Übergeordnetes Werk: |
volume:202 ; pages:103-113 |
| DOI / URN: |
10.1016/j.ecss.2017.12.012 |
|---|
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| 520 | |a A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. | ||
| 650 | 4 | |a Nutrient | |
| 650 | 4 | |a Chlorophyll | |
| 650 | 4 | |a Primary productivity | |
| 650 | 4 | |a Phytoplankton | |
| 650 | 4 | |a Liaodong Bay | |
| 650 | 4 | |a Liaohe River | |
| 700 | 1 | |a Laws, Edward A. |e verfasserin |4 aut | |
| 700 | 1 | |a Zhang, Haibo |e verfasserin |4 aut | |
| 700 | 1 | |a Ye, Siyuan |e verfasserin |4 aut | |
| 700 | 1 | |a Kemper, Marc T. |e verfasserin |4 aut | |
| 700 | 1 | |a Yuan, Hongming |e verfasserin |4 aut | |
| 700 | 1 | |a Xu, Gang |e verfasserin |4 aut | |
| 700 | 1 | |a Yang, Shixiong |e verfasserin |4 aut | |
| 700 | 1 | |a Liu, Haiyue |e verfasserin |4 aut | |
| 700 | 1 | |a Zhu, Yaxuan |e verfasserin |4 aut | |
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10.1016/j.ecss.2017.12.012 doi (DE-627)ELV000737895 (ELSEVIER)S0272-7714(17)31203-9 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.90 bkl 42.94 bkl Pei, Shaofeng verfasserin (orcid)0000-0001-5420-6264 aut Study on chemical hydrography, chlorophyll- 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River Laws, Edward A. verfasserin aut Zhang, Haibo verfasserin aut Ye, Siyuan verfasserin aut Kemper, Marc T. verfasserin aut Yuan, Hongming verfasserin aut Xu, Gang verfasserin aut Yang, Shixiong verfasserin aut Liu, Haiyue verfasserin aut Zhu, Yaxuan verfasserin aut Enthalten in Estuarine, coastal and shelf science London : Academic Press, 1981 202, Seite 103-113 Online-Ressource (DE-627)266016448 (DE-600)1466742-3 (DE-576)259270679 0272-7714 nnns volume:202 pages:103-113 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.90 Ozeanologie Ozeanographie 42.94 Meeresbiologie AR 202 103-113 |
| spelling |
10.1016/j.ecss.2017.12.012 doi (DE-627)ELV000737895 (ELSEVIER)S0272-7714(17)31203-9 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.90 bkl 42.94 bkl Pei, Shaofeng verfasserin (orcid)0000-0001-5420-6264 aut Study on chemical hydrography, chlorophyll- 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River Laws, Edward A. verfasserin aut Zhang, Haibo verfasserin aut Ye, Siyuan verfasserin aut Kemper, Marc T. verfasserin aut Yuan, Hongming verfasserin aut Xu, Gang verfasserin aut Yang, Shixiong verfasserin aut Liu, Haiyue verfasserin aut Zhu, Yaxuan verfasserin aut Enthalten in Estuarine, coastal and shelf science London : Academic Press, 1981 202, Seite 103-113 Online-Ressource (DE-627)266016448 (DE-600)1466742-3 (DE-576)259270679 0272-7714 nnns volume:202 pages:103-113 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.90 Ozeanologie Ozeanographie 42.94 Meeresbiologie AR 202 103-113 |
| allfields_unstemmed |
10.1016/j.ecss.2017.12.012 doi (DE-627)ELV000737895 (ELSEVIER)S0272-7714(17)31203-9 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.90 bkl 42.94 bkl Pei, Shaofeng verfasserin (orcid)0000-0001-5420-6264 aut Study on chemical hydrography, chlorophyll- 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River Laws, Edward A. verfasserin aut Zhang, Haibo verfasserin aut Ye, Siyuan verfasserin aut Kemper, Marc T. verfasserin aut Yuan, Hongming verfasserin aut Xu, Gang verfasserin aut Yang, Shixiong verfasserin aut Liu, Haiyue verfasserin aut Zhu, Yaxuan verfasserin aut Enthalten in Estuarine, coastal and shelf science London : Academic Press, 1981 202, Seite 103-113 Online-Ressource (DE-627)266016448 (DE-600)1466742-3 (DE-576)259270679 0272-7714 nnns volume:202 pages:103-113 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.90 Ozeanologie Ozeanographie 42.94 Meeresbiologie AR 202 103-113 |
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10.1016/j.ecss.2017.12.012 doi (DE-627)ELV000737895 (ELSEVIER)S0272-7714(17)31203-9 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.90 bkl 42.94 bkl Pei, Shaofeng verfasserin (orcid)0000-0001-5420-6264 aut Study on chemical hydrography, chlorophyll- 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River Laws, Edward A. verfasserin aut Zhang, Haibo verfasserin aut Ye, Siyuan verfasserin aut Kemper, Marc T. verfasserin aut Yuan, Hongming verfasserin aut Xu, Gang verfasserin aut Yang, Shixiong verfasserin aut Liu, Haiyue verfasserin aut Zhu, Yaxuan verfasserin aut Enthalten in Estuarine, coastal and shelf science London : Academic Press, 1981 202, Seite 103-113 Online-Ressource (DE-627)266016448 (DE-600)1466742-3 (DE-576)259270679 0272-7714 nnns volume:202 pages:103-113 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.90 Ozeanologie Ozeanographie 42.94 Meeresbiologie AR 202 103-113 |
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10.1016/j.ecss.2017.12.012 doi (DE-627)ELV000737895 (ELSEVIER)S0272-7714(17)31203-9 DE-627 ger DE-627 rda eng 550 DE-600 38.48 bkl 38.90 bkl 42.94 bkl Pei, Shaofeng verfasserin (orcid)0000-0001-5420-6264 aut Study on chemical hydrography, chlorophyll- 2017 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River Laws, Edward A. verfasserin aut Zhang, Haibo verfasserin aut Ye, Siyuan verfasserin aut Kemper, Marc T. verfasserin aut Yuan, Hongming verfasserin aut Xu, Gang verfasserin aut Yang, Shixiong verfasserin aut Liu, Haiyue verfasserin aut Zhu, Yaxuan verfasserin aut Enthalten in Estuarine, coastal and shelf science London : Academic Press, 1981 202, Seite 103-113 Online-Ressource (DE-627)266016448 (DE-600)1466742-3 (DE-576)259270679 0272-7714 nnns volume:202 pages:103-113 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_224 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.48 Marine Geologie 38.90 Ozeanologie Ozeanographie 42.94 Meeresbiologie AR 202 103-113 |
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English |
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Enthalten in Estuarine, coastal and shelf science 202, Seite 103-113 volume:202 pages:103-113 |
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Enthalten in Estuarine, coastal and shelf science 202, Seite 103-113 volume:202 pages:103-113 |
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Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River |
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Pei, Shaofeng @@aut@@ Laws, Edward A. @@aut@@ Zhang, Haibo @@aut@@ Ye, Siyuan @@aut@@ Kemper, Marc T. @@aut@@ Yuan, Hongming @@aut@@ Xu, Gang @@aut@@ Yang, Shixiong @@aut@@ Liu, Haiyue @@aut@@ Zhu, Yaxuan @@aut@@ |
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2017-01-01T00:00:00Z |
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550 DE-600 38.48 bkl 38.90 bkl 42.94 bkl Study on chemical hydrography, chlorophyll- Nutrient Chlorophyll Primary productivity Phytoplankton Liaodong Bay Liaohe River |
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Study on chemical hydrography, chlorophyll- |
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A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. |
| abstractGer |
A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. |
| abstract_unstemmed |
A field study was carried out during the summer of 2013 in Liaodong Bay, China to determine the dynamics of the phytoplankton in the bay and the extent to which primary production in the bay was constrained by environmental factors. There was little or no evidence of limitation of phytoplankton production by nutrient concentrations at any of the sampling stations, with the possible exception of a few offshore stations where phosphate concentrations were less than 30 nM. This assessment was consistent with the results of nutrient enrichment experiments and the values of light-saturated photosynthetic rates and areal photosynthetic rates. To examine the effects of irradiance and temperature on light-saturated photosynthetic rates normalized to chlorophyll a concentrations ( P o p t b ) at twelve stations where photosynthetic rates were measured by 14C method, light-conditioned values were modeled as a function of the temperature with a satisfactory fit to our field data (R 2 = 0.60, p = 0.003). According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. Areal production in Liaodong Bay appears to be controlled by a combination of temperature and light limitation. |
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According to this model, the light-conditioned P o p t b values increased with temperatures from 22 °C to roughly 25 °C but declined precipitously at higher temperatures, and P o p t b values and corresponding areal photosynthetic rates at all 66 stations were estimated to be 7.6 ± 2.4 g C g−1 Chl a h−1 and 532 ± 429 gC m−2 d−1 in average, respectively. The quanta absorbed per carbon atom fixed averaged 14 ± 2 and 37 ± 10 at six coastal stations and six estuarine stations, respectively. The relatively high P o p t b values and low quantum requirements at the coastal stations implied the highly efficient usage of absorbed light by phytoplankton under nutrient-replete conditions and favorable temperatures. Comparatively, the low P o p t b values and high quantum requirements at the estuarine stations suggested rather extreme light limitation and lowly efficient usage of absorbed light in photosynthesis in the Liaohe River estuary. 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