Enzymatically hydrolysed protein and carbohydrate pools in deep-sea sediments: estimates of the potentially bioavailable fraction and methodological considerations

By Antonio Dell'Anno, M. Fabiano, M. Mei, Roberto Danovaro. 2000

91 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/4fd77146c3bd690be7f056b43be892387d6627ac

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. M. Weintraub
2. D. Moorhead
3. R. Sinsabaugh
4. M. Wallenstein
5. A. Pusceddu
6. Cristina Gambi
7. Roberto Danovaro
8. Jack J. Middelburg

In Global and Planetary Change

1. Jack J. Middelburg
2. Roberto Danovaro
3. Cristina Gambi
4. A. Grémare
5. R. Sinsabaugh

In Oceanography

1. A. Pusceddu
2. Roberto Danovaro
3. Cristina Gambi
4. Jack J. Middelburg
5. D. Moorhead
6. A. Grémare
7. Carol Arnosti
8. E. Manini

Citations in the corpus

• Benthic microbial loop functioning in coastal lagoons: a comparative approach (2003, background): “It is recognised that the amount of available protein and carbohydrate pools in marine sediments (i.e., enzymatically hydrolysable, sensu Danovaro et al., 2001; Dell’Anno et al., 2000) is an important factor influencing bacterial activity and distribution (Danovaro et al., 1993, 1999a).”
• Extracellular enzymes in terrestrial, freshwater, and marine environments: perspectives on system variability and common research needs (2013, background): “20 cm of the sediment column, and only a handful of studies (e.g. Boetius and Lochte 1994, 1996; Boetius et al. 2000; Dell’Anno et al. 2000) come from surface sediments retrieved from the deep ocean.”
• Relationships between sedimentary organics and benthic meiofauna on the continental shelf and the upper slope of the Gulf of Lions (NW Mediterranean) (2002, methodology): “This is slightly higher than the protein concentrations (between 0.900 and 1.400 mg g–1 DW) recently reported for the Porcupine abyssal plain (Dell’Anno et al. 2000), but in the range of existing data regarding coastal sediments (i.e. <7.6 mg g–1 DW according to Dauwe et al. 1999).”
• Reviews and syntheses: to the bottom of carbon processing at the seafloor (2017, methodology): “…matter with various proxies such as the ratio of chlorophyll to bulk organic matter, fraction of nitrogen present as amino acids, and the contribution of proteins and carbohydrates to total organic matter (Cowie et al., 1992; Dell’Anno et al., 2000; Danovaro et al., 2001; Koho et al., 2013).”