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<md:lastName>van Kaam</md:lastName>
<md:firstName>Rianne J M</md:firstName>
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<md:year>2025</md:year>
<md:title>Total organic carbon and stable carbon isotopes of dust samples from ephemeral rivers in Namibia analyzed after the sorption experiment</md:title>
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<md:URI>https://doi.org/10.1594/PANGAEA.972505</md:URI>
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<md:author id="ref128613.author107322">
<md:lastName>van Kaam</md:lastName>
<md:firstName>Rianne J M</md:firstName>
<md:eMail>rvankaam@marum.de</md:eMail>
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<md:author id="ref128613.author672">
<md:lastName>Kölling</md:lastName>
<md:firstName>Martin</md:firstName>
<md:eMail>koelling@uni-bremen.de</md:eMail>
<md:URI>http://www.marum.de/Martin_Koelling.html</md:URI>
<md:orcid>0000-0003-2720-2211</md:orcid>
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<md:author id="ref128613.author27446">
<md:lastName>Elvert</md:lastName>
<md:firstName>Marcus</md:firstName>
<md:eMail>melvert@marum.de</md:eMail>
<md:orcid>0000-0003-3863-0975</md:orcid>
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<md:author id="ref128613.author23309">
<md:lastName>Hinrichs</md:lastName>
<md:firstName>Kai-Uwe</md:firstName>
<md:eMail>khinrichs@uni-bremen.de</md:eMail>
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<md:author id="ref128613.author626">
<md:lastName>Zabel</md:lastName>
<md:firstName>Matthias</md:firstName>
<md:eMail>mzabel@uni-bremen.de</md:eMail>
<md:orcid>0000-0003-4681-1821</md:orcid>
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<md:year>2025</md:year>
<md:title>Dust deposition directly affects the concentration of dissolved organic carbon in the ocean</md:title>
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<md:source id="ref128613.journal10808" relatedTermIds="33926,34022" type="journal">Marine Chemistry</md:source>
<md:volume>271</md:volume>
<md:URI>https://doi.org/10.1016/j.marchem.2025.104531</md:URI>
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<md:number>390741603</md:number>
<md:title>EXC 2077: The Ocean Floor – Earth's Uncharted Interface</md:title>
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<md:comment>Different amounts of dust (5 mg and 100 mg) were added to a mixture (30 mL) of artificial seawater and 13C-labeled Spirulina extract (~500 µM). Water samples were taken at multiple time points (0, 10, 24, 48, 72, 120, and 168 hours) and analyzed for DOC using a carbon analyzer (multiN/C 2100s, Analytik Jena). Dust samples were analyzed for TOC and δ13C-TOC before and after the experiments using isotope ratio mass spectrometry (IRMS) (Delta V Plus, Thermo Scientific, with a ConFlo IV interface to an elemental analyzer), calibrated against the Vienna Pee Dee Belemnite (VPDB) standard with a precision of ±0.35‰. After 72 hours, water samples were also analyzed for δ13C-DIC using isotope ratio infrared spectrometry (IRIS) with a universal reference interface (URI) (Delta Ray, Thermo Scientific), calibrated to the VPDB standard with a precision of ±0.05‰.</md:comment>
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<md:keyword id="keywords.term73571" type="fromDatabase">dissolved organic carbon (DOC)</md:keyword>
<md:keyword id="keywords.term74722" type="fromDatabase">Ephemeral river</md:keyword>
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