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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=20155"><dc:title>Editorial</dc:title><dc:creator>Guo,	Xianghui	(Avtor)
	</dc:creator><dc:creator>Bednaršek,	Nina	(Avtor)
	</dc:creator><dc:creator>Wang,	Hongjie	(Avtor)
	</dc:creator><dc:creator>Feely,	Richard Alan	(Avtor)
	</dc:creator><dc:creator>Arnaud,	Laurent	(Avtor)
	</dc:creator><dc:subject>coastal ecosystems</dc:subject><dc:subject>ocean acidification</dc:subject><dc:subject>zakisljevanje morja</dc:subject><dc:subject>biological impacts</dc:subject><dc:subject>hypoxia</dc:subject><dc:subject>hydrobiology</dc:subject><dc:description>Ocean acidification and hypoxia (dissolved oxygen &lt;2 mg L−1 or &lt;62 μmol L−1) are universal environmental concerns that can impact ecological and biogeochemical processes, including element cycling, carbon sequestration, community shifts, contributing to biodiversity reduction, and reducing marine ecosystem services (Riebesell et al., 2000; Feely et al., 2004, 2009; Andersson et al., 2005; Doney, 2006; Cohen and Holcomb, 2009; Doney et al., 2009, 2020; Kleypas and Yates, 2009; Ekstrom et al., 2015; Gattuso et al., 2015). While the stressors are global in their occurrence, local and regional impacts might be enhanced and even more accelerated, thus requiring even greater and faster consideration (Doney et al., 2020).</dc:description><dc:date>2022</dc:date><dc:date>2024-08-06 14:38:24</dc:date><dc:type>Neznano</dc:type><dc:identifier>20155</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
