• Keine Ergebnisse gefunden

The role of sea ice habitats in structuring the under-ice community during Antarctic winter

N/A
N/A
Protected

Academic year: 2022

Aktie "The role of sea ice habitats in structuring the under-ice community during Antarctic winter"

Copied!
1
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

INTRODUCTION Sea ice habitats are changing in some parts of the Antarctic Ocean. Sea ice hosts a specific algal community that can serve as a critical carbon source for juveniles Antarctic krill Euphausia superba and other species during winter. Therefore, changes of sea ice habitats can have a significant impact on ecosystem functioning. During a winter expedition in the Weddell Sea in 2013, we studied the community composition of under-ice fauna using a Surface and Under-Ice Trawl (SUIT) (in the upper image) equipped with a bio-environmental sensor array (CTD, altimeter, ADCP, video camera, two Hyperspectral radiometers ).

SEA ICE HABITATS

Thickness profiles (Fig.4) reveal differences of the under side of ice. An example where rough sea ice with the presence of ridges of 6-8m in station 565, contrasts with station 570 where flat ice dominates.

The role of sea ice habitats in structuring the under-ice community during Antarctic winter

Carmen David

1,2

, H. Flores

1,2

, B. Lange

1,2

, F. Schafsma

3

, J. van Franeker

3

1 Alfred Wegener Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Am Handelshafen 12, 27570,Bremerhaven, Germany

2 University Hamburg, Zoological Institute and Zoological Museum, Martin-Luther-King Platz 3,20146, Hamburg, Germany

3 IMARES Wageningen UR, 1790 AD Den Burg (Texel), The Netherlands

577 579

571 570

567 565

562 557 560

555 551

25° W 30° W

35° W 40° W

57° S

60° S

Ice concentration 16 Sept 2013

100%

0%

Fig.1 SUIT stations map; Sea ice concentration acquired from Bremen University (http://www.iup.uni-bremen.de: 8084/amsr/)); sampling was performed from west to east, from August to October 2013; stations color code correspond to the three ecotypes described on the left;

Fig.3 Principal component analysis on sea ice properties describing the under-ice habitats; stations color code correspond with the 3 ecotypes described above.

Fig.4 Sea ice thickness profiles of two SUIT hauls; photo made during trawling with the video camera attached to SUIT frame

Station 565

Station 570

SEA ICE HABITATS

Ice conditions varied spatially and seasonally. Higher ice concentration, thickness and roughness were encountered at the first stations and decrease to left on the PCA ordination (Fig.3). Snow thickness differentiates within groups’

stations ecotype II and ecotype III.

Graphics by GEO Grafik/Illuteam43

Fig.2 Cumulated abundance and biomass (dry weight) of the taxonomic groups in the SUIT stations

Ecotype I Ecotype II Ecotype III

UNDER-ICE FAUNA

Abundance and biomass differentiated 3 ecotypes

Differences in community are dictated by sea ice properties, with a strong seasonal signal

Antarctic krill (predominantly larvae) are associated with higher sea ice roughness

Higher species diversity is associated with thicker ice

CONCLUSION

More information on Iceflux project Ice-ecosystem carbon flux in polar oceans

Ecotype III

Low abundance Low biomass

Ecotype II

High Abundance Variable Biomass High diversity

Ecotype I

Dominance of krill Low Abundance High Biomass

Time Ice coverage, concentration, thickness

Referenzen

ÄHNLICHE DOKUMENTE

On the entire first north to south transect the surface ocean layer was well mixed down to 120 m water depth with salin-i---ties between 34.1 and 34.5 PSU.. A strong density gradient

In order to relate results obtained during the different time periods, empirical relationships are established between the length of the sea ice season, derived from the

This study presents profiles of the organic sulphur components dimethylsulfide (DMS) and dimethylsulfoniopropionate (DMSP) in sea ice cores collected during the

• Arctic cod and Antarctic krill may play similar key roles in transferring carbon from sea ice into the pelagic food web. • In both Polar Regions, sea ice-associated key species

The reliable relationship with the sampled distance estimated from the ship’s speed in water allowed the reconstruction of the distance of water sampled by SUIT

and colleagues conclude that, over the course of the twenty-first century, warm pulses of ocean currents are likely to reach this ice shelf and induce basal melt, whereas Ross

• Association of sea ice properties (thickness) with sympagic amphipods and polar cod and inversely correlated with association of water temperature and the amphipod T.libellula. •

In Section 4, the variations in the ridge height, spacing, ridging intensity and average thickness of ridged ice with increasing cutoff height are analyzed, and the