Carbon and nitrogen mineralization in sediments of the Bangrong mangrove area, Phuket, Thailand

By E. Kristensen, F. Andersen, N. Holmboe, M. Holmer, N. Thongtham. 2000

163 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/180181bb45aa333c6f2ffbc6fef281c8eeb799c5

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. E. Kristensen
2. D. Alongi
3. S. Bouillon
4. C. Marchand
5. T. Dittmar
6. J. Kostka
7. Thomas S. Bianchi
8. Jeffrey Chow

In Oceanography

1. E. Kristensen
2. D. Alongi
3. S. Bouillon
4. C. Marchand
5. T. Dittmar
6. J. Kostka
7. Thomas S. Bianchi
8. Jeffrey Chow

Citations in the corpus

• The role of terrestrially derived organic carbon in the coastal ocean: A changing paradigm and the priming effect (2011, background): “Increasing freshwater inputs will decrease residence time of TerrOC (both POC and DOC) to the Arctic Ocean, likely increasing inputs to the northern Atlantic; understanding the consequence of such changes will be a key part in understanding the changing global carbon cycle (72, 107).”
• Mangrove crabs as ecosystem engineers; with emphasis on sediment processes (2008, background): “Rates of microbial carbon oxidation in mangrove sediments typically range from 20 to 60 mmol m d (Kristensen et al., 2000; Alongi et al., 2001).”
• Effects of bioturbation and plant roots on salt marsh biogeochemistry: a mesocosm study (2002, background): “Thus, the enhanced carbon oxidation in the vegetated sediment is probably mediated by increased aerobic and iron respiration as found in other salt marsh and mangrove environments (Kristensen et al. 2000, Kostka et al. 2002).”
• Effects of bioturbation by root and crab activity on iron and sulfur biogeochemistry in mangrove substrate (2007, background): “, 1996) and suboxic respiration, the latter of which may use amorphous iron oxides as final electron acceptors (Kristensen et al., 2000).”
• Impact of Global Change on Nutrient Dynamics in Mangrove Forests (2018, background): “available nitrogen and phosphorus pools are short in keeping with the generally rapid rates of nutrient recycling [16].”
• Organic carbon dynamics in mangrove ecosystems : a review (2008, background): “Tidal DOC export from a Florida mangrove area (Twilley, 1985) was estimated to be 3.1–3.7 mol C m 2 year 1, while a mangrove tidal creek in Australia (Ayukai et al., 1998) exports 1.8 mol C m 2 year 1, and a mangrove forest in Thailand loses 0.6 mol C m 2 year 1 (Suraswadi, unpublished).”
• Recovery of novel bacterial diversity from mangrove sediment (2007, background): “It has been reported recently that iron reduction may be even more important for carbon and nitrogen mineralization in mangrove ecosystems (Kristensen et al. 2000).”
• Impact of fiddler crabs and plant roots on sediment biogeochemistry in a Georgia saltmarsh (2003, methodology): “The data obtained within the first 24 h were not included in the regressions used for TCO2 and Fe(II) rate determination due to disturbance of the sediment during homogenization (Kristensen et al. 2000).”
• Control by fiddler crabs (Uca vocans) and plant roots (Avicennia marina) on carbon, iron, and sulfur biogeochemistry in mangrove sediment (2006, background): “The partitioning observed here with dominance of FeR is comparable to results obtained for other iron-rich mangrove sediments (Kristensen et al. 2000) and saltmarshes (Kostka et al. 2002; Gribsholt et al. 2003), substantiating the potential importance of Fe(III) as electron acceptor in vegetated…”