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Concepción Shelf Sedimentation

Continental Shelf Sediment Dynamics Analysis (0-100m depth) by Claudio Iturra

Study Area: 36°S - 37°S, 73°W - 74°W

Shelf Width: ~15km | Max Depth: 100m

Sediment Sources: Biobío River, Coastal Erosion, Marine Production

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Average Rate

2.8 mm/yr

Holocene average across shelf

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Terrigenous Input

75%

River and coastal erosion

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Biogenic Input

25%

Marine productivity

Seasonal Variation

±40%

Winter vs summer rates

Sedimentation Rate vs Depth Profile

Depth Zone Analysis

Inner Shelf (0-30m)

High energy, coarse sediments

4.2 mm/yr

Mid Shelf (30-70m)

Moderate energy, mixed sediments

2.8 mm/yr

Outer Shelf (70-100m)

Low energy, fine sediments

1.5 mm/yr

Controlling Oceanographic Processes

🌊 Current-Driven Transport

  • • Peru-Chile Current: Northward transport
  • • Coastal undercurrent: Southward transport
  • • Cross-shelf exchange
  • • Tidal resuspension cycles

💨 Wind-Wave Effects

  • • Wave-induced bottom stress
  • • Seasonal storm resuspension
  • • Upwelling-driven circulation
  • • Ekman transport patterns

🏔️ Terrestrial Inputs

  • • Biobío River discharge
  • • Coastal cliff erosion
  • • Seasonal flood events
  • • Anthropogenic contributions

🦠 Biological Processes

  • • Upwelling-driven productivity
  • • Diatom blooms and settling
  • • Bioturbation effects
  • • Organic matter preservation

🌡️ Seasonal Cycles

  • • Winter storm intensification
  • • Summer upwelling maxima
  • • River discharge variability
  • • Temperature stratification

🌀 Climate Variability

  • • ENSO impact on sedimentation
  • • PDO long-term modulation
  • • Extreme event contributions
  • • Anthropocene acceleration