Abstract
Biological and sedimentologic samples along with X-radiographs of sediment slabs were taken from box cores in the HEBBLE area (4700 m) on the lower continental rise of Nova Scotia. These data suggest that this bottom region is influenced by periods of strong near-bottom currents which erode and physically transport sediments. These high periods alternate with periods of weaker flow. Biogenic reworking of sediments by an active benthic infauna dominates particle transport during low flow conditions.
| Original language | English |
|---|---|
| Pages (from-to) | M7-M15 |
| Journal | Marine Geology |
| Volume | 48 |
| Issue number | 1-2 |
| DOIs | |
| State | Published - Jul 1982 |
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