1997
DOI: 10.1023/a:1005806508707
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Cited by 54 publications
(3 citation statements)
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“…The highest concentrations of DON, DOP, POC, PN, and PP in seawater and N tot.. in sediment observed in June 1977 in PB was mostly the consequence of macrophyte decomposition after an intense growth illustrated by the high community production measured in April 1977. The high oxygen consumption of decomposing organic matter caused the night anoxia and the proliferation of sulphate reducing bacteria producing H 2 S and pyrite in sediments (Hines et al 1997).…”
Section: Discussionmentioning
confidence: 99%
“…The highest concentrations of DON, DOP, POC, PN, and PP in seawater and N tot.. in sediment observed in June 1977 in PB was mostly the consequence of macrophyte decomposition after an intense growth illustrated by the high community production measured in April 1977. The high oxygen consumption of decomposing organic matter caused the night anoxia and the proliferation of sulphate reducing bacteria producing H 2 S and pyrite in sediments (Hines et al 1997).…”
Section: Discussionmentioning
confidence: 99%
“…In order to define the KPIs for each scenario we have reviewed the relevant existing literature [Hines, Faganeli and Planinc, 1997;Kralj et al, 2019;Stachowitsch, 1984;Ingrosso, Giani, Cibic et al, 2016;Ingrosso, Giani, Comici et al, 2016;Ingrosso, Bensi et al, 2017;Cozzi and Giani, 2011;Giani et al, 2012;Mozetič et al, 2012;Brando et al, 2015;Cozzi, Falconi et al, 2012;Cossarini, Solidoro and Umani, 2012;Aubry et al, 2012].…”
Section: End Users Quality Indicatorsmentioning
confidence: 99%
“…26 Izotopska sestava 13 C DIC kaže, da je bentoški tok DIC večinoma organskega izvora in sicer v toplejšem (poletnem) obdobju izvira iz razgradnje razgradljivega organskega C sedimentiranega fitoplanktona in bentoških mikroalg, v hladnejšem (zimskem) obdobju pa iz razgradnje bolj odpornega (tudi kopenskega) sedimentiranega organskega C. V poletnem obdobju gostotne razslojenosti vodnega stolpa prihaja do intenzivne remineralizacije na meji sediment-voda, posebno v anoksičnih razmerah 27 , in oksidacije sulfida v H 2 SO 4 . 28 Takrat poteka omejeno raztapljanje karbonatov, ki prispeva približno 10% k toku DIC (slika 8). Podobne vrednosti (5%) so zasledili tudi ob obali italijanske dežele Emilia-Romagna.…”
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