Photosynthesis and light regime in the Azores Front region during summer: are light-saturated computations of primary production sufficient?
Bio-optical variables for primary production (PP) computations were determined at the Azores Front (AF) (30–38°N to 20–23°W) between 30 July and 21 August 1998. The area was characterized by the presence of a deep chlorophyll maximum (DCM) at ∼100 m and by high mesoscale variability in surface water...
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creator | Lorenzo, Luisa M Figueiras, Francisco G Tilstone, Gavin H Arbones, Belén Mirón, Iván |
description | Bio-optical variables for primary production (PP) computations were determined at the Azores Front (AF) (30–38°N to 20–23°W) between 30 July and 21 August 1998. The area was characterized by the presence of a deep chlorophyll maximum (DCM) at ∼100
m and by high mesoscale variability in surface waters caused by the meandering eastern flow of the Azores Current associated with the AF. The vertical distribution of the photosynthetic parameters was typical of oligotrophic waters with high values of light-limited slope (
α
B) and maximum quantum yield (
φ
m) at the DCM and high values of the chlorophyll-specific maximum photosynthetic rates (
P
m
B) at the surface. Spatial variability in photosynthetic parameters at the surface was high and comparable to that over larger spatial scales. Photosynthetic parameters at the surface associated with contrasting hydrographic structures were significantly different but at the DCM no significant differences were apparent. Although comparisons between the light absorbed by phytoplankton (
E
zPUR) and the corresponding spectral light saturation parameters (
E
kPUR) indicted that photosynthesis was light-limited during sunrise and sunset, integrated PP could be estimated using a simple light-saturated model (DLS model) that considers the day length equivalent for saturating irradiance of photosynthesis and the vertical distribution of
P
m
B and chlorophyll concentration. This means that PP computations for modeling could be greatly simplified by ignoring the spectral resolution and suggest that efforts in further research should be directed to characterize time and spatial variations of
P
m
B in these oligotrophic waters. |
doi_str_mv | 10.1016/j.dsr.2004.01.010 |
format | Article |
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m and by high mesoscale variability in surface waters caused by the meandering eastern flow of the Azores Current associated with the AF. The vertical distribution of the photosynthetic parameters was typical of oligotrophic waters with high values of light-limited slope (
α
B) and maximum quantum yield (
φ
m) at the DCM and high values of the chlorophyll-specific maximum photosynthetic rates (
P
m
B) at the surface. Spatial variability in photosynthetic parameters at the surface was high and comparable to that over larger spatial scales. Photosynthetic parameters at the surface associated with contrasting hydrographic structures were significantly different but at the DCM no significant differences were apparent. Although comparisons between the light absorbed by phytoplankton (
E
zPUR) and the corresponding spectral light saturation parameters (
E
kPUR) indicted that photosynthesis was light-limited during sunrise and sunset, integrated PP could be estimated using a simple light-saturated model (DLS model) that considers the day length equivalent for saturating irradiance of photosynthesis and the vertical distribution of
P
m
B and chlorophyll concentration. This means that PP computations for modeling could be greatly simplified by ignoring the spectral resolution and suggest that efforts in further research should be directed to characterize time and spatial variations of
P
m
B in these oligotrophic waters.</description><identifier>ISSN: 0967-0637</identifier><identifier>EISSN: 1879-0119</identifier><identifier>DOI: 10.1016/j.dsr.2004.01.010</identifier><language>eng</language><publisher>Oxford: Elsevier Ltd</publisher><subject>Azores Front ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Light ; Light regime ; Marine ; Photosynthesis ; Physics of the oceans ; Primary production ; Summer</subject><ispartof>Deep-sea research. Part I, Oceanographic research papers, 2004-09, Vol.51 (9), p.1229-1244</ispartof><rights>2004 Elsevier Ltd</rights><rights>2005 INIST-CNRS</rights><rights>Copyright Pergamon Press Inc. Sep 2004</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c449t-333356195c37b6294c569082189d3b6018e061583877877dd7ddd01d451b062a3</citedby><cites>FETCH-LOGICAL-c449t-333356195c37b6294c569082189d3b6018e061583877877dd7ddd01d451b062a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.dsr.2004.01.010$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=15989356$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Lorenzo, Luisa M</creatorcontrib><creatorcontrib>Figueiras, Francisco G</creatorcontrib><creatorcontrib>Tilstone, Gavin H</creatorcontrib><creatorcontrib>Arbones, Belén</creatorcontrib><creatorcontrib>Mirón, Iván</creatorcontrib><title>Photosynthesis and light regime in the Azores Front region during summer: are light-saturated computations of primary production sufficient?</title><title>Deep-sea research. Part I, Oceanographic research papers</title><description>Bio-optical variables for primary production (PP) computations were determined at the Azores Front (AF) (30–38°N to 20–23°W) between 30 July and 21 August 1998. The area was characterized by the presence of a deep chlorophyll maximum (DCM) at ∼100
m and by high mesoscale variability in surface waters caused by the meandering eastern flow of the Azores Current associated with the AF. The vertical distribution of the photosynthetic parameters was typical of oligotrophic waters with high values of light-limited slope (
α
B) and maximum quantum yield (
φ
m) at the DCM and high values of the chlorophyll-specific maximum photosynthetic rates (
P
m
B) at the surface. Spatial variability in photosynthetic parameters at the surface was high and comparable to that over larger spatial scales. Photosynthetic parameters at the surface associated with contrasting hydrographic structures were significantly different but at the DCM no significant differences were apparent. Although comparisons between the light absorbed by phytoplankton (
E
zPUR) and the corresponding spectral light saturation parameters (
E
kPUR) indicted that photosynthesis was light-limited during sunrise and sunset, integrated PP could be estimated using a simple light-saturated model (DLS model) that considers the day length equivalent for saturating irradiance of photosynthesis and the vertical distribution of
P
m
B and chlorophyll concentration. This means that PP computations for modeling could be greatly simplified by ignoring the spectral resolution and suggest that efforts in further research should be directed to characterize time and spatial variations of
P
m
B in these oligotrophic waters.</description><subject>Azores Front</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Light</subject><subject>Light regime</subject><subject>Marine</subject><subject>Photosynthesis</subject><subject>Physics of the oceans</subject><subject>Primary production</subject><subject>Summer</subject><issn>0967-0637</issn><issn>1879-0119</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNp9kU2LFDEQhhtRcFz9Ad6CoLceq_o7epBlcXeFBT3oOWSS9EyG7mRNpRfW3-CPtoYeEDwYXgiknrdSH0XxGmGLgN3749ZS2lYAzRaQBU-KDQ69LAFRPi02ILu-hK7unxcviI4AbBpgU_z-dog50mPIB0eehA5WTH5_yCK5vZ-d8EFwSFz-ismRuE4xrKEYhF2SD3tByzy79EHo5FZrSTovSWdnhYnz_ZJ1ZpxEHMV98rNOj3xHu5jTM9vH0RvvQv70sng26oncq_N9Ufy4_vz96ra8-3rz5eryrjRNI3NZ82k7lK2p-11Xyca0nYShwkHaetcBDg46bId66HuWtSwLaJsWd9BVur4o3q15uYyfi6OsZk_GTZMOLi6ksO9raHBg8M0_4DEuKXBtCnmg2NRtxRCukEmRKLlRnbtUCOq0HHVUvBx1Wo4CZAF73p4TazJ6GpMOxtNfYysHyT0y93HlHI_jwbuk6DQq46xPzmRlo__PL38AURyleg</recordid><startdate>20040901</startdate><enddate>20040901</enddate><creator>Lorenzo, Luisa M</creator><creator>Figueiras, Francisco G</creator><creator>Tilstone, Gavin H</creator><creator>Arbones, Belén</creator><creator>Mirón, Iván</creator><general>Elsevier Ltd</general><general>Elsevier</general><general>Pergamon Press Inc</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20040901</creationdate><title>Photosynthesis and light regime in the Azores Front region during summer: are light-saturated computations of primary production sufficient?</title><author>Lorenzo, Luisa M ; Figueiras, Francisco G ; Tilstone, Gavin H ; Arbones, Belén ; Mirón, Iván</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c449t-333356195c37b6294c569082189d3b6018e061583877877dd7ddd01d451b062a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Azores Front</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Light</topic><topic>Light regime</topic><topic>Marine</topic><topic>Photosynthesis</topic><topic>Physics of the oceans</topic><topic>Primary production</topic><topic>Summer</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lorenzo, Luisa M</creatorcontrib><creatorcontrib>Figueiras, Francisco G</creatorcontrib><creatorcontrib>Tilstone, Gavin H</creatorcontrib><creatorcontrib>Arbones, Belén</creatorcontrib><creatorcontrib>Mirón, Iván</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Deep-sea research. Part I, Oceanographic research papers</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lorenzo, Luisa M</au><au>Figueiras, Francisco G</au><au>Tilstone, Gavin H</au><au>Arbones, Belén</au><au>Mirón, Iván</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Photosynthesis and light regime in the Azores Front region during summer: are light-saturated computations of primary production sufficient?</atitle><jtitle>Deep-sea research. Part I, Oceanographic research papers</jtitle><date>2004-09-01</date><risdate>2004</risdate><volume>51</volume><issue>9</issue><spage>1229</spage><epage>1244</epage><pages>1229-1244</pages><issn>0967-0637</issn><eissn>1879-0119</eissn><abstract>Bio-optical variables for primary production (PP) computations were determined at the Azores Front (AF) (30–38°N to 20–23°W) between 30 July and 21 August 1998. The area was characterized by the presence of a deep chlorophyll maximum (DCM) at ∼100
m and by high mesoscale variability in surface waters caused by the meandering eastern flow of the Azores Current associated with the AF. The vertical distribution of the photosynthetic parameters was typical of oligotrophic waters with high values of light-limited slope (
α
B) and maximum quantum yield (
φ
m) at the DCM and high values of the chlorophyll-specific maximum photosynthetic rates (
P
m
B) at the surface. Spatial variability in photosynthetic parameters at the surface was high and comparable to that over larger spatial scales. Photosynthetic parameters at the surface associated with contrasting hydrographic structures were significantly different but at the DCM no significant differences were apparent. Although comparisons between the light absorbed by phytoplankton (
E
zPUR) and the corresponding spectral light saturation parameters (
E
kPUR) indicted that photosynthesis was light-limited during sunrise and sunset, integrated PP could be estimated using a simple light-saturated model (DLS model) that considers the day length equivalent for saturating irradiance of photosynthesis and the vertical distribution of
P
m
B and chlorophyll concentration. This means that PP computations for modeling could be greatly simplified by ignoring the spectral resolution and suggest that efforts in further research should be directed to characterize time and spatial variations of
P
m
B in these oligotrophic waters.</abstract><cop>Oxford</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.dsr.2004.01.010</doi><tpages>16</tpages></addata></record> |
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subjects | Azores Front Earth, ocean, space Exact sciences and technology External geophysics Light Light regime Marine Photosynthesis Physics of the oceans Primary production Summer |
title | Photosynthesis and light regime in the Azores Front region during summer: are light-saturated computations of primary production sufficient? |
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