Phosphate depletion in the western North Atlantic Ocean.
By Jingfeng Wu, W. Sunda, E. Boyle, David M. Karl. Science, 2000
808 citations recorded by the source corpus.
Subfields: Environmental Chemistry, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/c1fcb5e8bd22682a2c270d587591d0eacb9825d9
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Environmental Chemistry
- D. Capone
- C. Mahaffey
- David M. Karl
- Sonya T. Dyhrman
- Michael W. Lomas
- L. Naselli-Flores
- R. Barone
- Bess Ward
In Global and Planetary Change
- C. Mahaffey
- Sonya T. Dyhrman
- David M. Karl
- K. Björkman
- Michael W. Lomas
- Jordi Sardans
- J. Raven
- Albert Rivas‐Ubach
In Oceanography
- Sonya T. Dyhrman
- Michael J. Follows
- S. Dutkiewicz
- D. Capone
- M. Mulholland
- David M. Karl
- D. Hutchins
- Bess Ward
Citations in the corpus
- The elemental stoichiometry of aquatic and terrestrial ecosystems and its relationships with organismic lifestyle and ecosystem structure and function: a review and perspectives (2011, background): “The buffer effect of N2 fixers around Redfield’s ratio is dependent on the availability of elements other than N and P such as Fe and Mo, which are necessary for the enzymatic fixation of N2 (Howarth et al. 1988; Wu et al. 2000; Lenton and Watson 2000).”
- Iron requirements for dinitrogen‐ and ammonium‐supported growth in cultures of Trichodesmium (IMS 101): Comparison with nitrogen fixation rates and iron: carbon ratios of field populations (2003, background): “However, phosphorus has received increasing attention over the last few years as a potentially limiting nutrient for Trichodesmium (Wu et al. 2000; Sañudo-Wilhelmy et al. 2001), since a lack of P has been long known to limit freshwater diazotrophs in Fe-rich lakes.”
- Iron, phosphorus, and nitrogen supply ratios define the biogeography of nitrogen fixation (2013, background): “The system is controlled by wP:N only in limited regions, such as the North Atlantic (Wu et al. 2000; Moore et al. 2009; Palter et al. 2011), where wFe:N exceeds the demands of the diazotrophs.”
- A microbial source of phosphonates in oligotrophic marine systems (2009, background): “Phosphorus (P) has a key role in constraining the growth of marine primary producers over both modern and geologic timescale”
- Effect of nutrient amendments on bacterioplankton production, community structure, and DOC utilization in the northwestern Sargasso Sea (2002, background): “Extremely low inorganic phosphorus concentrations in the surface waters (Wu et al. 2000) would appear to support this hypothesis.”
- Phosphorus availability, phytoplankton community dynamics, and taxon‐specific phosphorus status in the Gulf of Aqaba, Red Sea (2006, background): “In the Sargasso Sea, orthophosphate (Pi) is suspected to play an important role in limiting production (Wu et al. 2000; Ammerman et al. 2003).”
- The Marine Nitrogen Cycle: Overview and Challenges (2008, background): “, 2005; Carpenter and Romans, 1991), yet these waters have extremely low PO 4 concentrations (Wu et al., 2000).”
- Diel variation of molybdenum and iron in marine diazotrophic cyanobacteria (2004, background): “Field measurements of C : N ratios in Trichodesmium from the North Atlantic and North Pacific are generally low, ranging from 4.7 to 7.3 (Letelier and Karl 1998; Berman-Frank et al. 2001a; Kustka et al. 2002).”
- Does competition for nanomolar phosphate supply explain the predominance of the cyanobacterium Synechococcus? (2002, methodology): “It has been proposed that primary production (Karl et al. 1997; Wu et al. 2000; Sañudo-Wilhelmy et al. 2001) as well as bacterial production (Thingstad and Rassoulzadegan 1999; Van Wambeke et al. 2002) are controlled by the availability of phosphate.”
- Rapid biologically mediated oxygen isotope exchange between water and phosphate (2002, background): “[2] Phosphorus (P) is considered to be a limiting nutrient in some oceanic systems [Karl et al., 1995; Cotner et al., 1997; Wu et al., 2000] and is possibly the ultimate limiting macronutrient for marine productivity over long timescales [Delaney, 1998; Tyrrell, 1999].”
- Iron and phosphorus co-limit nitrogen fixation in the eastern tropical North Atlantic (2004, result): “Oceanographic observations have been interpreted both to confirm and refute this hypothesi”
- Dynamics of Dissolved Organic Phosphorus (2015, methodology): “This method has been used to reliably detect subnanomolar concentrations of Pi in seawater (Wu et al., 2000).”
- Taxonomic variability of phosphorus stress in Sargasso Sea phytoplankton (2004, background): “…studies (Fanning 1992; Michaels et al. 1996) noted dissolved inorganic N : P ratios that were substantially greater than the canonical Redfield (1958) ratio, and that have recently been confirmed by high-sensitivity nutrient analytical methods (Wu et al. 2000; Cavender-Bares et al. 2001).”