Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay
The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in...
Ausführliche Beschreibung
Autor*in: |
Yiheng Wang [verfasserIn] Jianfang Chen [verfasserIn] Feng Zhou [verfasserIn] Wei Zhang [verfasserIn] Qiang Hao [verfasserIn] |
---|
Format: |
E-Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2022 |
---|
Schlagwörter: |
---|
Übergeordnetes Werk: |
In: Journal of Marine Science and Engineering - MDPI AG, 2014, 10(2022), 3, p 356 |
---|---|
Übergeordnetes Werk: |
volume:10 ; year:2022 ; number:3, p 356 |
Links: |
---|
DOI / URN: |
10.3390/jmse10030356 |
---|
Katalog-ID: |
DOAJ007903391 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | DOAJ007903391 | ||
003 | DE-627 | ||
005 | 20240414174037.0 | ||
007 | cr uuu---uuuuu | ||
008 | 230225s2022 xx |||||o 00| ||eng c | ||
024 | 7 | |a 10.3390/jmse10030356 |2 doi | |
035 | |a (DE-627)DOAJ007903391 | ||
035 | |a (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
050 | 0 | |a VM1-989 | |
050 | 0 | |a GC1-1581 | |
100 | 0 | |a Yiheng Wang |e verfasserin |4 aut | |
245 | 1 | 0 | |a Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay |
264 | 1 | |c 2022 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a Computermedien |b c |2 rdamedia | ||
338 | |a Online-Ressource |b cr |2 rdacarrier | ||
520 | |a The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. | ||
650 | 4 | |a Hangzhou Bay | |
650 | 4 | |a chlorophyll <i<a</i< | |
650 | 4 | |a primary productivity | |
650 | 4 | |a light exposure | |
650 | 4 | |a total suspended matters | |
653 | 0 | |a Naval architecture. Shipbuilding. Marine engineering | |
653 | 0 | |a Oceanography | |
700 | 0 | |a Jianfang Chen |e verfasserin |4 aut | |
700 | 0 | |a Feng Zhou |e verfasserin |4 aut | |
700 | 0 | |a Wei Zhang |e verfasserin |4 aut | |
700 | 0 | |a Qiang Hao |e verfasserin |4 aut | |
773 | 0 | 8 | |i In |t Journal of Marine Science and Engineering |d MDPI AG, 2014 |g 10(2022), 3, p 356 |w (DE-627)771274181 |w (DE-600)2738390-8 |x 20771312 |7 nnns |
773 | 1 | 8 | |g volume:10 |g year:2022 |g number:3, p 356 |
856 | 4 | 0 | |u https://doi.org/10.3390/jmse10030356 |z kostenfrei |
856 | 4 | 0 | |u https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 |z kostenfrei |
856 | 4 | 0 | |u https://www.mdpi.com/2077-1312/10/3/356 |z kostenfrei |
856 | 4 | 2 | |u https://doaj.org/toc/2077-1312 |y Journal toc |z kostenfrei |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_DOAJ | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_20 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_23 | ||
912 | |a GBV_ILN_24 | ||
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_95 | ||
912 | |a GBV_ILN_105 | ||
912 | |a GBV_ILN_110 | ||
912 | |a GBV_ILN_151 | ||
912 | |a GBV_ILN_161 | ||
912 | |a GBV_ILN_170 | ||
912 | |a GBV_ILN_213 | ||
912 | |a GBV_ILN_230 | ||
912 | |a GBV_ILN_285 | ||
912 | |a GBV_ILN_293 | ||
912 | |a GBV_ILN_370 | ||
912 | |a GBV_ILN_602 | ||
912 | |a GBV_ILN_2014 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4037 | ||
912 | |a GBV_ILN_4112 | ||
912 | |a GBV_ILN_4125 | ||
912 | |a GBV_ILN_4126 | ||
912 | |a GBV_ILN_4249 | ||
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_4335 | ||
912 | |a GBV_ILN_4338 | ||
912 | |a GBV_ILN_4367 | ||
912 | |a GBV_ILN_4700 | ||
951 | |a AR | ||
952 | |d 10 |j 2022 |e 3, p 356 |
author_variant |
y w yw j c jc f z fz w z wz q h qh |
---|---|
matchkey_str |
article:20771312:2022----::ptaadeprlaitosfhoohliinpiayrdc |
hierarchy_sort_str |
2022 |
callnumber-subject-code |
VM |
publishDate |
2022 |
allfields |
10.3390/jmse10030356 doi (DE-627)DOAJ007903391 (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Yiheng Wang verfasserin aut Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters Naval architecture. Shipbuilding. Marine engineering Oceanography Jianfang Chen verfasserin aut Feng Zhou verfasserin aut Wei Zhang verfasserin aut Qiang Hao verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 356 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 356 https://doi.org/10.3390/jmse10030356 kostenfrei https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 kostenfrei https://www.mdpi.com/2077-1312/10/3/356 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 356 |
spelling |
10.3390/jmse10030356 doi (DE-627)DOAJ007903391 (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Yiheng Wang verfasserin aut Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters Naval architecture. Shipbuilding. Marine engineering Oceanography Jianfang Chen verfasserin aut Feng Zhou verfasserin aut Wei Zhang verfasserin aut Qiang Hao verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 356 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 356 https://doi.org/10.3390/jmse10030356 kostenfrei https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 kostenfrei https://www.mdpi.com/2077-1312/10/3/356 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 356 |
allfields_unstemmed |
10.3390/jmse10030356 doi (DE-627)DOAJ007903391 (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Yiheng Wang verfasserin aut Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters Naval architecture. Shipbuilding. Marine engineering Oceanography Jianfang Chen verfasserin aut Feng Zhou verfasserin aut Wei Zhang verfasserin aut Qiang Hao verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 356 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 356 https://doi.org/10.3390/jmse10030356 kostenfrei https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 kostenfrei https://www.mdpi.com/2077-1312/10/3/356 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 356 |
allfieldsGer |
10.3390/jmse10030356 doi (DE-627)DOAJ007903391 (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Yiheng Wang verfasserin aut Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters Naval architecture. Shipbuilding. Marine engineering Oceanography Jianfang Chen verfasserin aut Feng Zhou verfasserin aut Wei Zhang verfasserin aut Qiang Hao verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 356 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 356 https://doi.org/10.3390/jmse10030356 kostenfrei https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 kostenfrei https://www.mdpi.com/2077-1312/10/3/356 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 356 |
allfieldsSound |
10.3390/jmse10030356 doi (DE-627)DOAJ007903391 (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 DE-627 ger DE-627 rakwb eng VM1-989 GC1-1581 Yiheng Wang verfasserin aut Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters Naval architecture. Shipbuilding. Marine engineering Oceanography Jianfang Chen verfasserin aut Feng Zhou verfasserin aut Wei Zhang verfasserin aut Qiang Hao verfasserin aut In Journal of Marine Science and Engineering MDPI AG, 2014 10(2022), 3, p 356 (DE-627)771274181 (DE-600)2738390-8 20771312 nnns volume:10 year:2022 number:3, p 356 https://doi.org/10.3390/jmse10030356 kostenfrei https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 kostenfrei https://www.mdpi.com/2077-1312/10/3/356 kostenfrei https://doaj.org/toc/2077-1312 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022 3, p 356 |
language |
English |
source |
In Journal of Marine Science and Engineering 10(2022), 3, p 356 volume:10 year:2022 number:3, p 356 |
sourceStr |
In Journal of Marine Science and Engineering 10(2022), 3, p 356 volume:10 year:2022 number:3, p 356 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters Naval architecture. Shipbuilding. Marine engineering Oceanography |
isfreeaccess_bool |
true |
container_title |
Journal of Marine Science and Engineering |
authorswithroles_txt_mv |
Yiheng Wang @@aut@@ Jianfang Chen @@aut@@ Feng Zhou @@aut@@ Wei Zhang @@aut@@ Qiang Hao @@aut@@ |
publishDateDaySort_date |
2022-01-01T00:00:00Z |
hierarchy_top_id |
771274181 |
id |
DOAJ007903391 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ007903391</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240414174037.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230225s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3390/jmse10030356</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ007903391</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJcbd80f15d201461b9158d74df8d90a02</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">VM1-989</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GC1-1581</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Yiheng Wang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hangzhou Bay</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">chlorophyll <i<a</i<</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">primary productivity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">light exposure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">total suspended matters</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Naval architecture. Shipbuilding. Marine engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Oceanography</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jianfang Chen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Feng Zhou</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Wei Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Qiang Hao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Marine Science and Engineering</subfield><subfield code="d">MDPI AG, 2014</subfield><subfield code="g">10(2022), 3, p 356</subfield><subfield code="w">(DE-627)771274181</subfield><subfield code="w">(DE-600)2738390-8</subfield><subfield code="x">20771312</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:10</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:3, p 356</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.3390/jmse10030356</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.mdpi.com/2077-1312/10/3/356</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2077-1312</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">10</subfield><subfield code="j">2022</subfield><subfield code="e">3, p 356</subfield></datafield></record></collection>
|
callnumber-first |
V - Naval Science |
author |
Yiheng Wang |
spellingShingle |
Yiheng Wang misc VM1-989 misc GC1-1581 misc Hangzhou Bay misc chlorophyll <i<a</i< misc primary productivity misc light exposure misc total suspended matters misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay |
authorStr |
Yiheng Wang |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)771274181 |
format |
electronic Article |
delete_txt_mv |
keep |
author_role |
aut aut aut aut aut |
collection |
DOAJ |
remote_str |
true |
callnumber-label |
VM1-989 |
illustrated |
Not Illustrated |
issn |
20771312 |
topic_title |
VM1-989 GC1-1581 Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay Hangzhou Bay chlorophyll <i<a</i< primary productivity light exposure total suspended matters |
topic |
misc VM1-989 misc GC1-1581 misc Hangzhou Bay misc chlorophyll <i<a</i< misc primary productivity misc light exposure misc total suspended matters misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography |
topic_unstemmed |
misc VM1-989 misc GC1-1581 misc Hangzhou Bay misc chlorophyll <i<a</i< misc primary productivity misc light exposure misc total suspended matters misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography |
topic_browse |
misc VM1-989 misc GC1-1581 misc Hangzhou Bay misc chlorophyll <i<a</i< misc primary productivity misc light exposure misc total suspended matters misc Naval architecture. Shipbuilding. Marine engineering misc Oceanography |
format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
cr |
hierarchy_parent_title |
Journal of Marine Science and Engineering |
hierarchy_parent_id |
771274181 |
hierarchy_top_title |
Journal of Marine Science and Engineering |
isfreeaccess_txt |
true |
familylinks_str_mv |
(DE-627)771274181 (DE-600)2738390-8 |
title |
Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay |
ctrlnum |
(DE-627)DOAJ007903391 (DE-599)DOAJcbd80f15d201461b9158d74df8d90a02 |
title_full |
Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay |
author_sort |
Yiheng Wang |
journal |
Journal of Marine Science and Engineering |
journalStr |
Journal of Marine Science and Engineering |
callnumber-first-code |
V |
lang_code |
eng |
isOA_bool |
true |
recordtype |
marc |
publishDateSort |
2022 |
contenttype_str_mv |
txt |
author_browse |
Yiheng Wang Jianfang Chen Feng Zhou Wei Zhang Qiang Hao |
container_volume |
10 |
class |
VM1-989 GC1-1581 |
format_se |
Elektronische Aufsätze |
author-letter |
Yiheng Wang |
doi_str_mv |
10.3390/jmse10030356 |
author2-role |
verfasserin |
title_sort |
spatial and temporal variations of chlorophyll <i<a</i< and primary productivity in the hangzhou bay |
callnumber |
VM1-989 |
title_auth |
Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay |
abstract |
The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. |
abstractGer |
The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. |
abstract_unstemmed |
The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations. |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 |
container_issue |
3, p 356 |
title_short |
Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay |
url |
https://doi.org/10.3390/jmse10030356 https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02 https://www.mdpi.com/2077-1312/10/3/356 https://doaj.org/toc/2077-1312 |
remote_bool |
true |
author2 |
Jianfang Chen Feng Zhou Wei Zhang Qiang Hao |
author2Str |
Jianfang Chen Feng Zhou Wei Zhang Qiang Hao |
ppnlink |
771274181 |
callnumber-subject |
VM - Naval Architecture, Shipbuilding, Marine Engineering |
mediatype_str_mv |
c |
isOA_txt |
true |
hochschulschrift_bool |
false |
doi_str |
10.3390/jmse10030356 |
callnumber-a |
VM1-989 |
up_date |
2024-07-03T14:48:36.567Z |
_version_ |
1803569716604698624 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ007903391</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240414174037.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230225s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.3390/jmse10030356</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ007903391</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJcbd80f15d201461b9158d74df8d90a02</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">VM1-989</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GC1-1581</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Yiheng Wang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Spatial and Temporal Variations of Chlorophyll <i<a</i< and Primary Productivity in the Hangzhou Bay</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll <i<a</i< (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m<sup<−3</sup< and 12.11 ± 12.25 mg C·m<sup<−3</sup<·h<sup<−1</sup<, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m<sup<−2</sup<·day<sup<−1</sup<) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P<sup<B</sup<) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P<sup<B</sup< period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hangzhou Bay</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">chlorophyll <i<a</i<</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">primary productivity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">light exposure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">total suspended matters</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Naval architecture. Shipbuilding. Marine engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Oceanography</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jianfang Chen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Feng Zhou</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Wei Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Qiang Hao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Journal of Marine Science and Engineering</subfield><subfield code="d">MDPI AG, 2014</subfield><subfield code="g">10(2022), 3, p 356</subfield><subfield code="w">(DE-627)771274181</subfield><subfield code="w">(DE-600)2738390-8</subfield><subfield code="x">20771312</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:10</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:3, p 356</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.3390/jmse10030356</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/cbd80f15d201461b9158d74df8d90a02</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://www.mdpi.com/2077-1312/10/3/356</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/2077-1312</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">10</subfield><subfield code="j">2022</subfield><subfield code="e">3, p 356</subfield></datafield></record></collection>
|
score |
7.40032 |