Ecological significance of benthic foraminifera: 13C labelling experiments

By L. Moodley, H. Boschker, Jack J. Middelburg, R. Pel, P. Herman, E. Deckere, Carlo H. R. Heip. 2000

211 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/3c754616f3db09e933f3015e9bc48f69cfdd64e6

How researchers see this paper

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

In Atmospheric Science

1. Jack J. Middelburg
2. Karline Soetaert
3. H. Boschker
4. Marco J. Houtekamer
5. Pieter van Rijswijk
6. Karel Van den Meersche
7. B. Veuger
8. Carlo H. R. Heip

In Ecology

1. Jack J. Middelburg
2. Karline Soetaert
3. B. Veuger
4. H. Boschker
5. Pieter van Rijswijk
6. L. Moodley
7. Karel Van den Meersche
8. Marco J. Houtekamer

In Oceanography

1. Jack J. Middelburg
2. Karline Soetaert
3. L. Moodley
4. H. Boschker
5. Pieter van Rijswijk
6. B. Veuger
7. Karel Van den Meersche
8. Carlo H. R. Heip

Citations in the corpus

• Oxygen as a control on sea floor biological communities and their roles in sedimentary carbon cycling (2007, background): “Previous isotope labeling studies in shallow coastal and deep-sea environments (Moodley et al. 2005) have concluded that the bacteria and foraminifera are responsible for a considerably greater percentage of OM uptake than the metazoan macrofauna (Moodley et al. 2000, 2002).”
• Analysis of 15N incorporation into D‐alanine: A new method for tracing nitrogen uptake by bacteria (2005, background): “The use of these membraneassociated compounds has yielded interesting results on bacterial and algal uptake of 13C-labeled substrates (Boschker et al. 1998; Middelburg et al. 2000; Moodley et al. 2000).”
• The fate of bacterial carbon in an intertidal sediment: Modeling an in situ isotope tracer experiment (2006, methodology): “DIC and 13C-DIC were determined by EA-IRMS (Moodley et al. 2000).”
• Carbon‐nitrogen coupling and algal‐bacterial interactions during an experimental bloom: Modeling a 13C tracer experiment (2004, methodology): “The incorporation of 13C in phytoplankton and bacterial biomass was quantified by carbon isotope analysis of specific PLFA using GC-combustion IRMS (Boschker and Middelburg 2002).”
• Stable isotopes and biomarkers in microbial ecology. (2002, methodology): “For food web studies it is now possible to study bacteria and other microorganisms like microalgae and fungi through biomarkers and larger organisms like nematodes and foraminifers can mostly be hand-picked and analysed directly [9,15].”