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Reviews and syntheses: Review of proxies for low-oxygen paleoceanographic reconstructions. <i>Biogeosciences 22(4)</i>: 863-957. <a href=\"https://dx.doi.org/10.5194/bg-22-863-2025\" target=\"_blank\">https://dx.doi.org/10.5194/bg-22-863-2025</a>","AutID":245916,"MonDate":null,"AnaDate":2025,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":437483,"RR":"<b>Karancz, S.; de Nooijer, L.J.; van der Wagt, B.; van der Meer, M.T.J.; Misra, S.; Hennekam, R.; Erdem, Z.; Lattaud, J.; Haghipour, N.; Schouten, S.; Reichart, G.-J.</b> (2025). Contrasts in the marine inorganic carbon chemistry of the Benguela Upwelling System since the Last Glacial Maximum. <i>Clim. Past 21(3)</i>: 679-704. <a href=\"https://dx.doi.org/10.5194/cp-21-679-2025\" target=\"_blank\">https://dx.doi.org/10.5194/cp-21-679-2025</a>","AutID":245916,"MonDate":null,"AnaDate":2025,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":393316,"RR":"<b>van Kemenade, Z.R.; Erdem, Z.; Hopmans, E.C.; Sinninghe Damsté, J.S; Rush, D.</b> (2024). Loss of nitrogen via anaerobic ammonium oxidation (anammox) in the California Current system during the late Quaternary. <i>Biogeosciences 21(6)</i>: 1517-1532. <a href=\"https://dx.doi.org/10.5194/bg-21-1517-2024\" target=\"_blank\">https://dx.doi.org/10.5194/bg-21-1517-2024</a>","AutID":245916,"MonDate":null,"AnaDate":2024,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":359687,"RR":"<b>Glock, N.; Erdem, Z.; Schönfeld, J.</b> (2022). The Peruvian oxygen minimum zone was similar in extent but weaker during the Last Glacial Maximum than Late Holocene. <i>Commun. Earth Environ. 3</i>: 307. <a href=\"https://dx.doi.org/10.1038/s43247-022-00635-y\" target=\"_blank\">https://dx.doi.org/10.1038/s43247-022-00635-y</a>","AutID":245916,"MonDate":null,"AnaDate":2022,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":359517,"RR":"<b>Lattaud, J.; Eglinton, T.I.; Tallon, M.; Bröder, L.; Erdem, Z.; Ausín, B.</b> (2022). Grain size controls on long-chain diol distributions and proxy signals in marine sediments. <i>Front. Mar. Sci. 9</i>: 1004096. <a href=\"https://dx.doi.org/10.3389/fmars.2022.1004096\" target=\"_blank\">https://dx.doi.org/10.3389/fmars.2022.1004096</a>","AutID":245916,"MonDate":null,"AnaDate":2022,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":348431,"RR":"<b>Erdem, Z.; Lattaud, J.; van Erk, M.R.; Mezger, E.M.; Reichart, G.-J.; Lückge, A.; Sinninghe Damste, J.S.; Schouten, S.</b> (2021). Applicability of the long chain diol index (LDI) as a sea surface temperature proxy in the Arabian Sea. <i>Paleoceanography and Paleoclimatology 36(12)</i>: e2021PA004255. <a href=\"https://dx.doi.org/10.1029/2021pa004255\" target=\"_blank\">https://dx.doi.org/10.1029/2021pa004255</a>","AutID":245916,"MonDate":null,"AnaDate":2021,"PeerRev":1,"outputType":"1_A1","OpenAcc":0},{"BRefID":328431,"RR":"<b>Erdem, Z.; Schönfeld, J.; Rathburn, A.E.; Pérez, M.-E.; Cardich, J.; Glock, N.</b> (2020). Bottom-water deoxygenation at the Peruvian margin during the last deglaciation recorded by benthic foraminifera. <i>Biogeosciences 17(12)</i>: 3165-3182. <a href=\"https://dx.doi.org/10.5194/bg-17-3165-2020\" target=\"_blank\">https://dx.doi.org/10.5194/bg-17-3165-2020</a>","AutID":245916,"MonDate":null,"AnaDate":2020,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":314337,"RR":"<b>Lattaud, J.; Erdem, Z.; Weiss, G.M.; Rush, D.; Balzano, S.; Chivall, D.; van der Meer, M.T.J.; Hopmans, E.C.; Sinninghe Damsté, J.S; Schouten, S.</b> (2019). Hydrogen isotopic ratios of long-chain diols reflect salinity. <i>Org. Geochem. 137</i>: 103904. <a href=\"https://dx.doi.org/10.1016/j.orggeochem.2019.103904\" target=\"_blank\">https://dx.doi.org/10.1016/j.orggeochem.2019.103904</a>","AutID":245916,"MonDate":null,"AnaDate":2019,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":294652,"RR":"<b>Glock, N.; Erdem, Z.; Wallmann, K.; Somes, C.J.; Liebetrau, V.; Schönfeld, J.; Gorb, S.; Eisenhauer, A.</b> (2018). Coupling of oceanic carbon and nitrogen facilitates spatially resolved quantitative reconstruction of nitrate inventories. <i>Nature Comm. 9(1)</i>: 10 pp. <a href=\"https://doi.org/10.1038/s41467-018-03647-5\" target=\"_blank\">https://doi.org/10.1038/s41467-018-03647-5</a>","AutID":245916,"MonDate":null,"AnaDate":2018,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":291452,"RR":"<b>Erdem, Z.; Schönfeld, J.</b> (2017). Pleistocene to Holocene benthic foraminiferal assemblages from the Peruvian continental margin. <i>Palaeontologia Electronica 20(2)</i>: 35A. <a href=\"https://doi.org/10.26879/764\" target=\"_blank\">https://doi.org/10.26879/764</a>","AutID":245916,"MonDate":null,"AnaDate":2017,"PeerRev":1,"outputType":"1_A1","OpenAcc":1},{"BRefID":281998,"RR":"<b>Doering, K.; Erdem, Z.; Ehlert, C.; Fleury, S.; Frank, M.; Schneider, R.</b> (2016). Changes in diatom productivity and upwelling intensity off Peru since the Last Glacial Maximum: Response to basin-scale atmospheric and oceanic forcing. <i>Paleoceanography 31</i>: 1453–1473. <a href=\"http://dx.doi.org/10.1002/2016PA002936\" target=\"_blank\">dx.doi.org/10.1002/2016PA002936</a>","AutID":245916,"MonDate":null,"AnaDate":2016,"PeerRev":1,"outputType":"1_A1","OpenAcc":1}],"Report":[{"BRefID":304783,"RR":"<b>Rush, D.; Erdem, Z.</b> (2018). 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