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. 2016 Aug 29;6(18):6662–6671. doi: 10.1002/ece3.2408

Table 1.

Mean generation rates of particulate and dissolved organic matter (POM and DOM), burial and respiration rates in hard and soft substrate coastal habitats

Habitat POM/DOM generation rate (g C m−2 day−1) Burial rate (g C m−2 day−1) Respiration rate(g C m−2 day−1)
POM DOM
Seaweed 0.8a 0.4b 5.8c
Mangroves 0.5a 0.3d 0.4e 5.1c
Salt marshes 0.2f 0.3f 0.6e 5.5c
Coral reefs 0.1g 0.4g 4.3c
Sea grasses 0.3a 0.1b 0.4e 1.9c
Sediments 0.2b 0.03f 0.001h 0.03c , i

Most hard substrate habitats such as seaweed and coral reefs do not bury carbon as the hard substratum makes burial impossible (Duarte et al., 2013).

a

Cebrian (2002).

b

Barrón et al. (2012).

c

Middelburg, Duarte, and Gattuso (2005).

d

Maher et al. (2013).

e

Duarte et al. (2013).

f

Maher and Eyre (2010).

g

Nakajima et al. (2010).

h

Oakes and Eyre (2014). Estimated from 13C‐bicarbonate incorporation into sediments.

i

Using the exponential relationship between sediment respiration versus depth (Middelburg et al., 2005); Respiration = 32e−0.0077z, where z is water depth (m), we are including shallow coastal habitats down to 20 m water depth.