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Preface The expedition ARK XIX/3 with the German icebreaking RV ...

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ounding processes as well. One possibility is that coastal wave activity rounded <strong>the</strong><br />

clasts, as it can be actually observed e.g. at <strong>the</strong> Isfjorden coast near Longyearbyen.<br />

Ano<strong>the</strong>r possibility is that glaciers advanced over extensive sander plains and this<br />

sandy and gravelly material was entrained in moraines during later glacier<br />

readvances. Today this is not observable on Spitsbergen. During <strong>the</strong> lowstand of <strong>the</strong><br />

last glacial maximum (ca. 18 kyr BP) this may have occurred on <strong>the</strong> shelf around<br />

Svålbard. In sou<strong>the</strong>rn Scandinavia this was a widely active landscape forming<br />

process.<br />

17 % of <strong>the</strong> clasts are incrusted by bryozoa, serpulid tubes, calcareous sponges or<br />

rare foraminifers. Most of <strong>the</strong>se clasts are siliciclastic sediments (90 %), less frequent<br />

are metamorphics (7 %, mainly fine quartzites), volcanics (1 %) and bituminous<br />

siltstones, limestones and chalk (2 %), but none are plutonic rocks. Some clasts show<br />

incrustation on all sides of <strong>the</strong> clasts, indicating low sedimentation rates and<br />

occasional rotation of <strong>the</strong> clasts by bioturbation or sediment reworking. Most bryozoa<br />

shells are damaged and only <strong>the</strong> part in contact <strong>with</strong> <strong>the</strong> clast is preserved, except<br />

when <strong>the</strong> bryozoa were protected from abrasion in small cavities.<br />

<strong>The</strong> surface of many clasts, most of <strong>the</strong>m incrusted, is often entirely or partly darker<br />

than <strong>the</strong> interior due to Mn-oxide and Fe-hydroxide precipitation. On <strong>the</strong>se Mn-oxide<br />

covered clasts <strong>the</strong> skeletons of bryozoa and <strong>the</strong> tubes of serpulids have orange<br />

colours (siderite?) whereas on o<strong>the</strong>r clasts <strong>the</strong>y are white (calcite). Probably <strong>the</strong> Mnoxides<br />

and Fe-hydroxides were formed in <strong>the</strong> upper part of <strong>the</strong> sediments under<br />

suboxic or changing oxic and reducing conditions.<br />

On average <strong>the</strong> material consists of 4 % plutonic %, 1 % volcanic, 73 % sedimentary<br />

and 22 % metamorphic rocks and this distribution does not vary much between<br />

sampling sites (Fig. C5-1). Description of various rock types:<br />

Plutonic rocks: unrounded quartz, unrounded feldspar, granite /<br />

granodiorite, diorite / gabbro.<br />

Volcanic rocks: basalt <strong>with</strong> or <strong>with</strong>out bubbles, pumice.<br />

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