Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial

Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the s...
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Autor*in:	Miao Chen [verfasserIn] Xiaoxiao Zhao [verfasserIn] Da-Wei Li [verfasserIn] Liang Dong [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	archaeal ammonia oxidation nitrogen fixation GDGTs the last glacial period mesoscale eddies northern South China Sea

Übergeordnetes Werk:	In: Frontiers in Earth Science - Frontiers Media S.A., 2014, 10(2022)
Übergeordnetes Werk:	volume:10 ; year:2022

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3389/feart.2022.886200

Katalog-ID:	DOAJ043085288

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520			\|a Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the spatial pattern of the role of archaeal ammonia oxidation in the SCS, the GDGT-[2]/[3] ratio (Glycerol Dialkyl Glycerol Tetraether), an indicator of the archaeal ammonia oxidation rate, was analyzed and examined from the collected data profiles since the last glacial period in the northern SCS. The results showed that the GDGT-[2]/[3] ratio in the northern SCS was opposite to that in the southern SCS, with higher GDGT-[2]/[3] values during the Holocene compared to the last glacial period. Based on existing published depths of thermocline (DOT) data in the northern SCS since 30 ka, we believe that hydrological structural variations induced by mesoscale eddies caused this difference. Therefore, physical processes are very important factors that control the nitrogen cycle over a long-time scale. This study may provide new insights into the understanding of the role of archaeal ammonia oxidation within the marine nitrogen cycle over geological time scale.
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spelling	10.3389/feart.2022.886200 doi (DE-627)DOAJ043085288 (DE-599)DOAJ0b75b83dc6e94a198773aefa169dc121 DE-627 ger DE-627 rakwb eng Miao Chen verfasserin aut Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the spatial pattern of the role of archaeal ammonia oxidation in the SCS, the GDGT-[2]/[3] ratio (Glycerol Dialkyl Glycerol Tetraether), an indicator of the archaeal ammonia oxidation rate, was analyzed and examined from the collected data profiles since the last glacial period in the northern SCS. The results showed that the GDGT-[2]/[3] ratio in the northern SCS was opposite to that in the southern SCS, with higher GDGT-[2]/[3] values during the Holocene compared to the last glacial period. Based on existing published depths of thermocline (DOT) data in the northern SCS since 30 ka, we believe that hydrological structural variations induced by mesoscale eddies caused this difference. Therefore, physical processes are very important factors that control the nitrogen cycle over a long-time scale. This study may provide new insights into the understanding of the role of archaeal ammonia oxidation within the marine nitrogen cycle over geological time scale. archaeal ammonia oxidation nitrogen fixation GDGTs the last glacial period mesoscale eddies northern South China Sea Science Q Xiaoxiao Zhao verfasserin aut Xiaoxiao Zhao verfasserin aut Da-Wei Li verfasserin aut Da-Wei Li verfasserin aut Liang Dong verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 10(2022) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:10 year:2022 https://doi.org/10.3389/feart.2022.886200 kostenfrei https://doaj.org/article/0b75b83dc6e94a198773aefa169dc121 kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2022.886200/full kostenfrei https://doaj.org/toc/2296-6463 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_2003 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022
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allfieldsSound	10.3389/feart.2022.886200 doi (DE-627)DOAJ043085288 (DE-599)DOAJ0b75b83dc6e94a198773aefa169dc121 DE-627 ger DE-627 rakwb eng Miao Chen verfasserin aut Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the spatial pattern of the role of archaeal ammonia oxidation in the SCS, the GDGT-[2]/[3] ratio (Glycerol Dialkyl Glycerol Tetraether), an indicator of the archaeal ammonia oxidation rate, was analyzed and examined from the collected data profiles since the last glacial period in the northern SCS. The results showed that the GDGT-[2]/[3] ratio in the northern SCS was opposite to that in the southern SCS, with higher GDGT-[2]/[3] values during the Holocene compared to the last glacial period. Based on existing published depths of thermocline (DOT) data in the northern SCS since 30 ka, we believe that hydrological structural variations induced by mesoscale eddies caused this difference. Therefore, physical processes are very important factors that control the nitrogen cycle over a long-time scale. This study may provide new insights into the understanding of the role of archaeal ammonia oxidation within the marine nitrogen cycle over geological time scale. archaeal ammonia oxidation nitrogen fixation GDGTs the last glacial period mesoscale eddies northern South China Sea Science Q Xiaoxiao Zhao verfasserin aut Xiaoxiao Zhao verfasserin aut Da-Wei Li verfasserin aut Da-Wei Li verfasserin aut Liang Dong verfasserin aut In Frontiers in Earth Science Frontiers Media S.A., 2014 10(2022) (DE-627)771399731 (DE-600)2741235-0 22966463 nnns volume:10 year:2022 https://doi.org/10.3389/feart.2022.886200 kostenfrei https://doaj.org/article/0b75b83dc6e94a198773aefa169dc121 kostenfrei https://www.frontiersin.org/articles/10.3389/feart.2022.886200/full kostenfrei https://doaj.org/toc/2296-6463 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_2003 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2022
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topic_facet	archaeal ammonia oxidation nitrogen fixation GDGTs the last glacial period mesoscale eddies northern South China Sea Science Q
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container_title	Frontiers in Earth Science
authorswithroles_txt_mv	Miao Chen @@aut@@ Xiaoxiao Zhao @@aut@@ Da-Wei Li @@aut@@ Liang Dong @@aut@@
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author	Miao Chen
spellingShingle	Miao Chen misc archaeal ammonia oxidation misc nitrogen fixation misc GDGTs misc the last glacial period misc mesoscale eddies misc northern South China Sea misc Science misc Q Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial
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topic_title	Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial archaeal ammonia oxidation nitrogen fixation GDGTs the last glacial period mesoscale eddies northern South China Sea
topic	misc archaeal ammonia oxidation misc nitrogen fixation misc GDGTs misc the last glacial period misc mesoscale eddies misc northern South China Sea misc Science misc Q
topic_unstemmed	misc archaeal ammonia oxidation misc nitrogen fixation misc GDGTs misc the last glacial period misc mesoscale eddies misc northern South China Sea misc Science misc Q
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title	Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial
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title_full	Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial
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title_sort	mesoscale eddy effects on nitrogen cycles in the northern south china sea since the last glacial
title_auth	Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial
abstract	Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the spatial pattern of the role of archaeal ammonia oxidation in the SCS, the GDGT-[2]/[3] ratio (Glycerol Dialkyl Glycerol Tetraether), an indicator of the archaeal ammonia oxidation rate, was analyzed and examined from the collected data profiles since the last glacial period in the northern SCS. The results showed that the GDGT-[2]/[3] ratio in the northern SCS was opposite to that in the southern SCS, with higher GDGT-[2]/[3] values during the Holocene compared to the last glacial period. Based on existing published depths of thermocline (DOT) data in the northern SCS since 30 ka, we believe that hydrological structural variations induced by mesoscale eddies caused this difference. Therefore, physical processes are very important factors that control the nitrogen cycle over a long-time scale. This study may provide new insights into the understanding of the role of archaeal ammonia oxidation within the marine nitrogen cycle over geological time scale.
abstractGer	Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the spatial pattern of the role of archaeal ammonia oxidation in the SCS, the GDGT-[2]/[3] ratio (Glycerol Dialkyl Glycerol Tetraether), an indicator of the archaeal ammonia oxidation rate, was analyzed and examined from the collected data profiles since the last glacial period in the northern SCS. The results showed that the GDGT-[2]/[3] ratio in the northern SCS was opposite to that in the southern SCS, with higher GDGT-[2]/[3] values during the Holocene compared to the last glacial period. Based on existing published depths of thermocline (DOT) data in the northern SCS since 30 ka, we believe that hydrological structural variations induced by mesoscale eddies caused this difference. Therefore, physical processes are very important factors that control the nitrogen cycle over a long-time scale. This study may provide new insights into the understanding of the role of archaeal ammonia oxidation within the marine nitrogen cycle over geological time scale.
abstract_unstemmed	Archaeal ammonia oxidation is the most important intermediate pathway in regulating the oceanic nitrogen cycle; however, the study of its specific role on a geological time scale is restricted to a specific part of marginal seas; thus far, only in the southern South China Sea (SCS). To explore the spatial pattern of the role of archaeal ammonia oxidation in the SCS, the GDGT-[2]/[3] ratio (Glycerol Dialkyl Glycerol Tetraether), an indicator of the archaeal ammonia oxidation rate, was analyzed and examined from the collected data profiles since the last glacial period in the northern SCS. The results showed that the GDGT-[2]/[3] ratio in the northern SCS was opposite to that in the southern SCS, with higher GDGT-[2]/[3] values during the Holocene compared to the last glacial period. Based on existing published depths of thermocline (DOT) data in the northern SCS since 30 ka, we believe that hydrological structural variations induced by mesoscale eddies caused this difference. Therefore, physical processes are very important factors that control the nitrogen cycle over a long-time scale. This study may provide new insights into the understanding of the role of archaeal ammonia oxidation within the marine nitrogen cycle over geological time scale.
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title_short	Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial
url	https://doi.org/10.3389/feart.2022.886200 https://doaj.org/article/0b75b83dc6e94a198773aefa169dc121 https://www.frontiersin.org/articles/10.3389/feart.2022.886200/full https://doaj.org/toc/2296-6463
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Mesoscale Eddy Effects on Nitrogen Cycles in the Northern South China Sea Since the Last Glacial

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