Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable
Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM...
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Gespeichert in:
| Autor*in: |
Modenutti, Beatriz [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Basel 2012 |
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| Übergeordnetes Werk: |
Enthalten in: Aquatic sciences - SP Birkhäuser Verlag Basel, 1989, 75(2012), 3 vom: 10. Nov., Seite 361-371 |
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| Übergeordnetes Werk: |
volume:75 ; year:2012 ; number:3 ; day:10 ; month:11 ; pages:361-371 |
| Links: |
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| DOI / URN: |
10.1007/s00027-012-0282-3 |
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OLC2068824299 |
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| 520 | |a Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. | ||
| 650 | 4 | |a Light climate | |
| 650 | 4 | |a Lakes | |
| 650 | 4 | |a Chlorophyll distribution | |
| 650 | 4 | |a Transparent lakes | |
| 650 | 4 | |a Climate change | |
| 650 | 4 | |a Total suspended solids | |
| 700 | 1 | |a Balseiro, Esteban |4 aut | |
| 700 | 1 | |a Bastidas Navarro, Marcela |4 aut | |
| 700 | 1 | |a Laspoumaderes, Cecilia |4 aut | |
| 700 | 1 | |a Souza, María Sol |4 aut | |
| 700 | 1 | |a Cuassolo, Florencia |4 aut | |
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10.1007/s00027-012-0282-3 doi (DE-627)OLC2068824299 (DE-He213)s00027-012-0282-3-p DE-627 ger DE-627 rakwb eng 550 VZ 570 550 VZ 12 14 13 21,3 ssgn BIODIV DE-30 fid 42.00 bkl Modenutti, Beatriz verfasserin aut Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel 2012 Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. Light climate Lakes Chlorophyll distribution Transparent lakes Climate change Total suspended solids Balseiro, Esteban aut Bastidas Navarro, Marcela aut Laspoumaderes, Cecilia aut Souza, María Sol aut Cuassolo, Florencia aut Enthalten in Aquatic sciences SP Birkhäuser Verlag Basel, 1989 75(2012), 3 vom: 10. Nov., Seite 361-371 (DE-627)130758795 (DE-600)1000078-1 (DE-576)023035080 1015-1621 nnns volume:75 year:2012 number:3 day:10 month:11 pages:361-371 https://doi.org/10.1007/s00027-012-0282-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2012 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4082 GBV_ILN_4277 GBV_ILN_4319 42.00 VZ AR 75 2012 3 10 11 361-371 |
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10.1007/s00027-012-0282-3 doi (DE-627)OLC2068824299 (DE-He213)s00027-012-0282-3-p DE-627 ger DE-627 rakwb eng 550 VZ 570 550 VZ 12 14 13 21,3 ssgn BIODIV DE-30 fid 42.00 bkl Modenutti, Beatriz verfasserin aut Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel 2012 Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. Light climate Lakes Chlorophyll distribution Transparent lakes Climate change Total suspended solids Balseiro, Esteban aut Bastidas Navarro, Marcela aut Laspoumaderes, Cecilia aut Souza, María Sol aut Cuassolo, Florencia aut Enthalten in Aquatic sciences SP Birkhäuser Verlag Basel, 1989 75(2012), 3 vom: 10. Nov., Seite 361-371 (DE-627)130758795 (DE-600)1000078-1 (DE-576)023035080 1015-1621 nnns volume:75 year:2012 number:3 day:10 month:11 pages:361-371 https://doi.org/10.1007/s00027-012-0282-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2012 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4082 GBV_ILN_4277 GBV_ILN_4319 42.00 VZ AR 75 2012 3 10 11 361-371 |
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10.1007/s00027-012-0282-3 doi (DE-627)OLC2068824299 (DE-He213)s00027-012-0282-3-p DE-627 ger DE-627 rakwb eng 550 VZ 570 550 VZ 12 14 13 21,3 ssgn BIODIV DE-30 fid 42.00 bkl Modenutti, Beatriz verfasserin aut Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel 2012 Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. Light climate Lakes Chlorophyll distribution Transparent lakes Climate change Total suspended solids Balseiro, Esteban aut Bastidas Navarro, Marcela aut Laspoumaderes, Cecilia aut Souza, María Sol aut Cuassolo, Florencia aut Enthalten in Aquatic sciences SP Birkhäuser Verlag Basel, 1989 75(2012), 3 vom: 10. Nov., Seite 361-371 (DE-627)130758795 (DE-600)1000078-1 (DE-576)023035080 1015-1621 nnns volume:75 year:2012 number:3 day:10 month:11 pages:361-371 https://doi.org/10.1007/s00027-012-0282-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2012 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4082 GBV_ILN_4277 GBV_ILN_4319 42.00 VZ AR 75 2012 3 10 11 361-371 |
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10.1007/s00027-012-0282-3 doi (DE-627)OLC2068824299 (DE-He213)s00027-012-0282-3-p DE-627 ger DE-627 rakwb eng 550 VZ 570 550 VZ 12 14 13 21,3 ssgn BIODIV DE-30 fid 42.00 bkl Modenutti, Beatriz verfasserin aut Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel 2012 Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. Light climate Lakes Chlorophyll distribution Transparent lakes Climate change Total suspended solids Balseiro, Esteban aut Bastidas Navarro, Marcela aut Laspoumaderes, Cecilia aut Souza, María Sol aut Cuassolo, Florencia aut Enthalten in Aquatic sciences SP Birkhäuser Verlag Basel, 1989 75(2012), 3 vom: 10. Nov., Seite 361-371 (DE-627)130758795 (DE-600)1000078-1 (DE-576)023035080 1015-1621 nnns volume:75 year:2012 number:3 day:10 month:11 pages:361-371 https://doi.org/10.1007/s00027-012-0282-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2012 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4082 GBV_ILN_4277 GBV_ILN_4319 42.00 VZ AR 75 2012 3 10 11 361-371 |
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10.1007/s00027-012-0282-3 doi (DE-627)OLC2068824299 (DE-He213)s00027-012-0282-3-p DE-627 ger DE-627 rakwb eng 550 VZ 570 550 VZ 12 14 13 21,3 ssgn BIODIV DE-30 fid 42.00 bkl Modenutti, Beatriz verfasserin aut Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable 2012 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Basel 2012 Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. Light climate Lakes Chlorophyll distribution Transparent lakes Climate change Total suspended solids Balseiro, Esteban aut Bastidas Navarro, Marcela aut Laspoumaderes, Cecilia aut Souza, María Sol aut Cuassolo, Florencia aut Enthalten in Aquatic sciences SP Birkhäuser Verlag Basel, 1989 75(2012), 3 vom: 10. Nov., Seite 361-371 (DE-627)130758795 (DE-600)1000078-1 (DE-576)023035080 1015-1621 nnns volume:75 year:2012 number:3 day:10 month:11 pages:361-371 https://doi.org/10.1007/s00027-012-0282-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_252 GBV_ILN_267 GBV_ILN_2003 GBV_ILN_2012 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4082 GBV_ILN_4277 GBV_ILN_4319 42.00 VZ AR 75 2012 3 10 11 361-371 |
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environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable |
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Environmental changes affecting light climate in oligotrophic mountain lakes: the deep chlorophyll maxima as a sensitive variable |
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Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. © Springer Basel 2012 |
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Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. © Springer Basel 2012 |
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Abstract The North-Patagonian Andean lakes of Argentina are high light, low nutrient environments that exhibit development of deep chlorophyll maxima (DCM) at the metalimnetic layer during summer stratification, at approximately 1 % of surface PAR irradiance. We examined whether the position of DCM changes as a consequence of long-time (global warming: glacial clay input) and short-time (eruption: volcanic ashes) events. We performed different field studies: (1) an interlacustrine analysis of six lakes from different basins, including data of the 2011 volcanic eruption, which caused an unexpected variation in water transparency; and (2) an intralacustrine analysis in which we compared different stations along a transparency gradient in Lake Mascardi caused by glacial clay input at one end of the gradient. In these analyses, we documented changes in DCM depth and its relationship with different parameters. DCM development was not related with thermocline depth or nutrient distribution. In all cases, the only significant variables were Kd 320 nm and Kd PAR. Our study showed that suspended particles (glacial clay and volcanic ashes) can play a crucial role in transparent lakes, affecting lake features such as the phototrophic biomass distribution along the water column. Suspended solid inputs from either glacial clay or volcanic ashes produce a comparable effect, provoking a decrease in light and, consequently, an upper location of the DCM. Thus, the DCM position is highly sensitive to global changes, such as increased temperatures causing glacier recession or to regional changes caused by volcanic eruptions. © Springer Basel 2012 |
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