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Variation in Riverine Inputs Affect Dissolved Organic Matter Characteristics throughout the Estuarine Gradient. / Asmala, Eero; Kaartokallio, Hermanni; Carstensen, Jacob et al.
In: Frontiers in Marine Science, Vol. 2, 125, 12.01.2016.

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Asmala, E, Kaartokallio, H, Carstensen, J & Thomas, DN 2016, 'Variation in Riverine Inputs Affect Dissolved Organic Matter Characteristics throughout the Estuarine Gradient', Frontiers in Marine Science, vol. 2, 125. https://doi.org/doi.org/10.3389/fmars.2015.00125

APA

Asmala, E., Kaartokallio, H., Carstensen, J., & Thomas, D. N. (2016). Variation in Riverine Inputs Affect Dissolved Organic Matter Characteristics throughout the Estuarine Gradient. Frontiers in Marine Science, 2, Article 125. https://doi.org/doi.org/10.3389/fmars.2015.00125

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MLA

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Asmala E, Kaartokallio H, Carstensen J, Thomas DN. Variation in Riverine Inputs Affect Dissolved Organic Matter Characteristics throughout the Estuarine Gradient. Frontiers in Marine Science. 2016 Jan 12;2:125. doi: doi.org/10.3389/fmars.2015.00125

Author

Asmala, Eero ; Kaartokallio, Hermanni ; Carstensen, Jacob et al. / Variation in Riverine Inputs Affect Dissolved Organic Matter Characteristics throughout the Estuarine Gradient. In: Frontiers in Marine Science. 2016 ; Vol. 2.

RIS

TY - JOUR

T1 - Variation in Riverine Inputs Affect Dissolved Organic Matter Characteristics throughout the Estuarine Gradient

AU - Asmala, Eero

AU - Kaartokallio, Hermanni

AU - Carstensen, Jacob

AU - Thomas, David N.

PY - 2016/1/12

Y1 - 2016/1/12

N2 - Terrestrial dissolved organic matter (DOM) undergoes significant changes during the estuarine transport from river mouths to the open sea. These include transformations and degradation by biological and chemical processes, but also the production of fresh organic matter. Since many of these processes occur simultaneously, properties of the DOM pool represent the net changes during the passage along the hydrological path. We examined changes in multiple DOM characteristics across three Finnish estuarine gradients during spring, summer and autumn: Dissolved organic carbon (DOC) concentration, colored DOM absorbance and fluorescence, stable carbon isotope signal of DOC, and molecular size distribution. Changes in these DOM characteristics with salinity were analyzed in relation to residence time (i.e., freshwater transit time), since increased residence time is likely to enhance DOM degradation while stimulating autochthonous DOM production at the same time. Our results show that the investigated DOM characteristics are highly correlated, indicating common physico-chemical transformations along the salinity continuum. Residence time did not explain variations in the DOM characteristics any better than salinity. Due to large variations in DOM characteristics at the river end-member, conservative mixing models do not seem to be able to accurately describe the occurrence and extent of deviations in DOM properties in the estuaries we investigated.

AB - Terrestrial dissolved organic matter (DOM) undergoes significant changes during the estuarine transport from river mouths to the open sea. These include transformations and degradation by biological and chemical processes, but also the production of fresh organic matter. Since many of these processes occur simultaneously, properties of the DOM pool represent the net changes during the passage along the hydrological path. We examined changes in multiple DOM characteristics across three Finnish estuarine gradients during spring, summer and autumn: Dissolved organic carbon (DOC) concentration, colored DOM absorbance and fluorescence, stable carbon isotope signal of DOC, and molecular size distribution. Changes in these DOM characteristics with salinity were analyzed in relation to residence time (i.e., freshwater transit time), since increased residence time is likely to enhance DOM degradation while stimulating autochthonous DOM production at the same time. Our results show that the investigated DOM characteristics are highly correlated, indicating common physico-chemical transformations along the salinity continuum. Residence time did not explain variations in the DOM characteristics any better than salinity. Due to large variations in DOM characteristics at the river end-member, conservative mixing models do not seem to be able to accurately describe the occurrence and extent of deviations in DOM properties in the estuaries we investigated.

UR - http://journal.frontiersin.org/article/10.3389/fmars.2015.00125/full

U2 - doi.org/10.3389/fmars.2015.00125

DO - doi.org/10.3389/fmars.2015.00125

M3 - Article

VL - 2

JO - Frontiers in Marine Science

JF - Frontiers in Marine Science

SN - 2296-7745

M1 - 125

ER -