Revising the nitrogen cycle in the Peruvian oxygen minimum zone

By P. Lam, G. Lavik, M. Jensen, J. van de Vossenberg, M. Schmid, D. Woebken, D. Gutiérrez, R. Amann, M. Jetten, M. Kuypers. Proceedings of the National Academy of Sciences of the United States of America, 2009

761 citations recorded by the source corpus.

Subfields: Ecology, Oceanography, Pollution

View Paper: https://www.semanticscholar.org/paper/b2d846e123cbd402a94dbdc38099311e9c4fd622

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Citations in the corpus

Microbial Nitrogen Cycling in Estuaries: From Genes to Ecosystem Processes (2018, background): “However, numerous functional genes have since emerged (Table 1): Scalindua-like nirS (Lam et al. 2009), which codes for a nitrite reductase specific to Scalindua bacteria, the dominant anammox bacteria in marine OMZs (Kuypers et al.”
Nitrogenase genes in non-cyanobacterial plankton: prevalence, diversity and regulation in marine waters (2010, background): “The OMZs account for 8% of the global ocean area and play an essential role in the global N cycle (Paulmier & RuizPino 2009), primarily due to loss of fixed N through denitrification (e.g. Ward et al. 2009) and anaerobic ammonia oxidation (e.g. Lam et al. 2009).”
Zooplankton in the eastern tropical north Pacific: Boundary effects of oxygen minimum zone expansion (2013, neutral): “OMZs are important in global biogeochemical cycles and the biological pump (e.g. Lam et al., 2009; Kalvelage et al., 2011).”
Anammox and denitrification in the oxygen minimum zone of the eastern South Pacific (2012, methodology): “Here we report results of the investigation of the processes responsible for removal of fixed nitrogen in the ETSP and into subtropical waters along the coasts of Chile and Peru between 26uS and 12uS.”
Heterotrophic nitrifying bacteria in wastewater biological nitrogen removal systems: A review (2021, background): “…the gene abundance of AOB (Pan, Gao, Fan, et al., 2018; Pan, Gao, Li, et al., 2018), AOA (Pan, Gao, Fan, et al., 2018; Pan, Gao, Li, et al., 2018), comammox bacteria (Pan, Gao, Fan, et al., 2018; Pjevac et al., 2017), and anaerobic AOB (Lam et al., 2009; Wang et al., 2012) by qPCR /: not mentioned.”
Quantification of ammonia oxidation rates and ammonia‐oxidizing archaea and bacteria at high resolution in the Gulf of California and eastern tropical North Pacific Ocean (2012, background): “…greater than most maximum ammonia oxidation rates reported in the literature, such as 288 nmol L21 d21 in the eastern tropical South Pacific (ETSP; Lipschultz et al. 1990), 283 nmol L21 d21 in the ETSP (Ward et al. 1989a), 262 nmol L21 d21 in the Benguela upwelling region (Rees et al. 2006), 210…”
Ammonia oxidation rates and nitrification in the Arabian Sea (2011, background): “[28] It has been suggested that ammonia oxidation in the oxycline supports anaerobic ammonia oxidation (anammox) [Lam et al., 2009].”
Autotrophic Ammonia Removal Processes: Ecology to Technology (2012, background): “Oceanic OMZs are responsible for about 35% of the oceanic N2 production and almost half of it comes from anaerobic activity in the Arabian Sea and Eastern Tropical South Pacific (ETSP; Lam et al., 2009, Ward et al., 2009).”
Activity, abundance and community structure of anammox bacteria along depth profiles in three different paddy soils (2015, background): “For instance, the genus Candidatus Scalindua was frequently discovered in marine ecosystems (Lam et al., 2009; Humbert et al., 2010; Dang et al., 2013), while Candidatus Brocadia and Kuenenia were mainly detected in soil and freshwater ecosystems (Sonthiphand et al.”