|
Titel |
Macrofaunal colonization across the Indian margin oxygen minimum zone |
VerfasserIn |
L. A. Levin, A. L. McGregor, G. F. Mendoza, C. Woulds, P. Cross, U. Witte, A. J. Gooday, G. Cowie, H. Kitazato |
Medientyp |
Artikel
|
Sprache |
Englisch
|
ISSN |
1726-4170
|
Digitales Dokument |
URL |
Erschienen |
In: Biogeosciences ; 10, no. 11 ; Nr. 10, no. 11 (2013-11-12), S.7161-7177 |
Datensatznummer |
250085406
|
Publikation (Nr.) |
copernicus.org/bg-10-7161-2013.pdf |
|
|
|
Zusammenfassung |
There is a growing need to understand the ability of bathyal assemblages to
recover from disturbance and oxygen stress, as human activities and expanding
oxygen minimum zones increasingly affect deep continental margins. The
effects of a pronounced oxygen minimum zone (OMZ) on slope benthic community
structure have been studied on every major upwelling margin; however, little
is known about the dynamics or resilience of these benthic populations. To
examine the influence of oxygen and phytodetritus on short-term settlement
patterns, we conducted colonization experiments at 3 depths on the West
Indian continental margin. Four colonization trays were deployed at each
depth for 4 days at 542 and 802 m (transect 1–16°58' N) and for
9 days at 817 and 1147 m (transect 2–17°31' N). Oxygen
concentrations ranged from 0.9 μM (0.02 mL L−1) at 542 m to
22 μM (0.5 mL L−1) at 1147 m. All trays contained local
defaunated sediments; half of the trays at each depth also contained
13C/15N-labeled phytodetritus mixed into the sediments.
Sediment cores were collected between 535 m and 1140 m from 2 cross-margin
transects for analysis of ambient (source) macrofaunal
(>300 μm) densities and composition. Ambient macrofaunal
densities ranged from 0 ind m−2 (at 535–542 m) to
7400 ind m−2, with maximum values on both transects at 700–800 m.
Macrofaunal colonizer densities ranged from 0 ind m−2 at 542 m, where
oxygen was lowest, to average values of 142 ind m−2 at 800 m, and
3074 ind m−2 at 1147 m, where oxygen concentration was highest.
These were equal to 4.3 and 151% of the ambient community at 800 m and
1147 m, respectively. Community structure of settlers showed no response to
the presence of phytodetritus. Increasing depth and oxygen concentration,
however, significantly influenced the community composition and abundance of
colonizing macrofauna. Polychaetes constituted 92.4% of the total
colonizers, followed by crustaceans (4.2%), mollusks (2.5%), and
echinoderms (0.8%). The majority of colonizers were found at 1147 m;
88.5% of these were Capitella sp., although they were rare in
the ambient community. Colonists at 800 and 1147 m also included ampharetid,
spionid, syllid, lumbrinerid, cirratulid, cossurid and sabellid polychaetes.
Consumption of 13C/15N-labeled phytodetritus was observed for
macrofaunal foraminifera (too large to be colonizers) at the 542 and
802/817 m sites, and by metazoan macrofauna mainly at the deepest, better
oxygenated sites. Calcareous foraminifera (Uvigerina,
Hoeglundina sp.), capitellid polychaetes and cumaceans were among
the major phytodetritus consumers. These preliminary experiments suggest that
bottom-water oxygen concentrations may strongly influence ecosystem services
on continental margins, as reflected in rates of colonization by benthos and
colonizer processing of carbon following disturbance. They may also provide a
window into future patterns of settlement on the continental slope as the
world's oxygen minimum zones expand. |
|
|
Teil von |
|
|
|
|
|
|