TY - JOUR
T1 - Macrofaunal control of microbial community structure in continental margin sediments
AU - Deng, Longhui
AU - Bölsterli, Damian
AU - Kristensen, Erik
AU - Meile, Christof
AU - Su, Chih-Chieh
AU - Bernasconi, Stefano Michele
AU - Seidenkrantz, Marit-Solveig
AU - Glombitza, Clemens
AU - Lagostina, Lorenzo
AU - Han, Xingguo
AU - Jørgensen, Bo Barker
AU - Røy, Hans
AU - Lever, Mark Alexander
N1 - Copyright © 2020 the Author(s). Published by PNAS.
PY - 2020/7
Y1 - 2020/7
N2 - Through a process called "bioturbation," burrowing macrofauna have altered the seafloor habitat and modified global carbon cycling since the Cambrian. However, the impact of macrofauna on the community structure of microorganisms is poorly understood. Here, we show that microbial communities across bioturbated, but geochemically and sedimentologically divergent, continental margin sites are highly similar but differ clearly from those in nonbioturbated surface and underlying subsurface sediments. Solid- and solute-phase geochemical analyses combined with modeled bioturbation activities reveal that dissolved O2 introduction by burrow ventilation is the major driver of archaeal community structure. By contrast, solid-phase reworking, which regulates the distribution of fresh, algal organic matter, is the main control of bacterial community structure. In nonbioturbated surface sediments and in subsurface sediments, bacterial and archaeal communities are more divergent between locations and appear mainly driven by site-specific differences in organic carbon sources.
AB - Through a process called "bioturbation," burrowing macrofauna have altered the seafloor habitat and modified global carbon cycling since the Cambrian. However, the impact of macrofauna on the community structure of microorganisms is poorly understood. Here, we show that microbial communities across bioturbated, but geochemically and sedimentologically divergent, continental margin sites are highly similar but differ clearly from those in nonbioturbated surface and underlying subsurface sediments. Solid- and solute-phase geochemical analyses combined with modeled bioturbation activities reveal that dissolved O2 introduction by burrow ventilation is the major driver of archaeal community structure. By contrast, solid-phase reworking, which regulates the distribution of fresh, algal organic matter, is the main control of bacterial community structure. In nonbioturbated surface sediments and in subsurface sediments, bacterial and archaeal communities are more divergent between locations and appear mainly driven by site-specific differences in organic carbon sources.
KW - Bioturbation
KW - Burrow ventilation
KW - Organic carbon sources
KW - Particle reworking
KW - Redox state
UR - http://www.scopus.com/inward/record.url?scp=85088207530&partnerID=8YFLogxK
U2 - 10.1073/pnas.1917494117
DO - 10.1073/pnas.1917494117
M3 - Journal article
C2 - 32576690
SN - 0027-8424
VL - 117
SP - 15911
EP - 15922
JO - Proceedings of the National Academy of Sciences (PNAS)
JF - Proceedings of the National Academy of Sciences (PNAS)
IS - 27
ER -