Details
| Original language | English |
|---|---|
| Pages (from-to) | 605-624 |
| Number of pages | 20 |
| Journal | The Depositional Record |
| Volume | 6 |
| Issue number | 3 |
| Early online date | 25 Mar 2020 |
| Publication status | Published - 27 Sept 2020 |
| Externally published | Yes |
Abstract
Submarine fans are formed by sediment-laden flows shed from continental margins into ocean basins. Their morphology represents the interplay of external controls such as tectonics, climate and sea level with internal processes including channel migration and lobe compensation. However, the nature of this interaction is poorly understood. Physical modelling was used to represent the evolution of a natural-scale submarine fan deposited during an externally forced waxing-to-waning sediment supply cycle. This was achieved by running five successive experimental turbidity currents with incrementally increasing then decreasing sediment supply rates. Deposits built upon the deposits of earlier flows and the distribution of erosion and deposition after each flow was recorded using digital elevation models. Initially, increasing sediment supply rate (waxing phase) led to widening and deepening of the slope channel, with basin-floor deposits compensationally stepping forwards into the basin, favouring topographic lows. When sediment supply rate was decreased (waning phase), the slope-channel filled as the bulk of the deposit abruptly back-stepped due to interaction with depositional topography. Therefore, despite flows in the waxing and waning phases of sediment supply having nominally identical input conditions (i.e. sediment concentration, supply rate, grain size, etc.), depositional relief led to development of markedly different deposits. This demonstrates how external controls can be preserved in the depositional record through the progradation of basin floor deposits but that internal processes such as compensational stacking progressively obscure this signal through time. This evolution serves as an additional potential mechanism to explain commonly observed coarsening and thickening-upwards lobe deposits, with abrupt transition to thin fine-grained deposits. Meanwhile within the slope channel, external forcing was more readily detectable through time, with less internally driven reorganization. This validates many existing conceptual models and outcrop observations that channels are more influenced by external forcing whilst internal processes dominate basin floor lobe deposits in submarine fans.
Keywords
- Allogenic, autogenic, experimental modelling, sediment gravity flow, submarine fan architecture
ASJC Scopus subject areas
- Environmental Science(all)
- Environmental Science (miscellaneous)
- Earth and Planetary Sciences(all)
- Geology
- Earth and Planetary Sciences(all)
- Oceanography
- Earth and Planetary Sciences(all)
- Palaeontology
- Earth and Planetary Sciences(all)
- Stratigraphy
Sustainable Development Goals
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In: The Depositional Record, Vol. 6, No. 3, 27.09.2020, p. 605-624.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Entangled external and internal controls on submarine fan evolution
T2 - an experimental perspective
AU - Ferguson, Ross A.
AU - Kane, Ian A.
AU - Eggenhuisen, Joris T.
AU - Pohl, Florian
AU - Tilston, Mike
AU - Spychala, Yvonne T.
AU - Brunt, Rufus L.
N1 - Publisher Copyright: © 2020 The Authors. The Depositional Record published by John Wiley & Sons Ltd on behalf of International Association of Sedimentologists.
PY - 2020/9/27
Y1 - 2020/9/27
N2 - Submarine fans are formed by sediment-laden flows shed from continental margins into ocean basins. Their morphology represents the interplay of external controls such as tectonics, climate and sea level with internal processes including channel migration and lobe compensation. However, the nature of this interaction is poorly understood. Physical modelling was used to represent the evolution of a natural-scale submarine fan deposited during an externally forced waxing-to-waning sediment supply cycle. This was achieved by running five successive experimental turbidity currents with incrementally increasing then decreasing sediment supply rates. Deposits built upon the deposits of earlier flows and the distribution of erosion and deposition after each flow was recorded using digital elevation models. Initially, increasing sediment supply rate (waxing phase) led to widening and deepening of the slope channel, with basin-floor deposits compensationally stepping forwards into the basin, favouring topographic lows. When sediment supply rate was decreased (waning phase), the slope-channel filled as the bulk of the deposit abruptly back-stepped due to interaction with depositional topography. Therefore, despite flows in the waxing and waning phases of sediment supply having nominally identical input conditions (i.e. sediment concentration, supply rate, grain size, etc.), depositional relief led to development of markedly different deposits. This demonstrates how external controls can be preserved in the depositional record through the progradation of basin floor deposits but that internal processes such as compensational stacking progressively obscure this signal through time. This evolution serves as an additional potential mechanism to explain commonly observed coarsening and thickening-upwards lobe deposits, with abrupt transition to thin fine-grained deposits. Meanwhile within the slope channel, external forcing was more readily detectable through time, with less internally driven reorganization. This validates many existing conceptual models and outcrop observations that channels are more influenced by external forcing whilst internal processes dominate basin floor lobe deposits in submarine fans.
AB - Submarine fans are formed by sediment-laden flows shed from continental margins into ocean basins. Their morphology represents the interplay of external controls such as tectonics, climate and sea level with internal processes including channel migration and lobe compensation. However, the nature of this interaction is poorly understood. Physical modelling was used to represent the evolution of a natural-scale submarine fan deposited during an externally forced waxing-to-waning sediment supply cycle. This was achieved by running five successive experimental turbidity currents with incrementally increasing then decreasing sediment supply rates. Deposits built upon the deposits of earlier flows and the distribution of erosion and deposition after each flow was recorded using digital elevation models. Initially, increasing sediment supply rate (waxing phase) led to widening and deepening of the slope channel, with basin-floor deposits compensationally stepping forwards into the basin, favouring topographic lows. When sediment supply rate was decreased (waning phase), the slope-channel filled as the bulk of the deposit abruptly back-stepped due to interaction with depositional topography. Therefore, despite flows in the waxing and waning phases of sediment supply having nominally identical input conditions (i.e. sediment concentration, supply rate, grain size, etc.), depositional relief led to development of markedly different deposits. This demonstrates how external controls can be preserved in the depositional record through the progradation of basin floor deposits but that internal processes such as compensational stacking progressively obscure this signal through time. This evolution serves as an additional potential mechanism to explain commonly observed coarsening and thickening-upwards lobe deposits, with abrupt transition to thin fine-grained deposits. Meanwhile within the slope channel, external forcing was more readily detectable through time, with less internally driven reorganization. This validates many existing conceptual models and outcrop observations that channels are more influenced by external forcing whilst internal processes dominate basin floor lobe deposits in submarine fans.
KW - Allogenic
KW - autogenic
KW - experimental modelling
KW - sediment gravity flow
KW - submarine fan architecture
UR - http://www.scopus.com/inward/record.url?scp=85089256783&partnerID=8YFLogxK
U2 - 10.1002/dep2.109
DO - 10.1002/dep2.109
M3 - Article
VL - 6
SP - 605
EP - 624
JO - The Depositional Record
JF - The Depositional Record
SN - 2055-4877
IS - 3
ER -