4.8 Article

Meltwater sediment transport as the dominating process in mid-latitude trough mouth fan formation

期刊

NATURE COMMUNICATIONS
卷 11, 期 1, 页码 -

出版社

NATURE PORTFOLIO
DOI: 10.1038/s41467-020-18337-4

关键词

-

资金

  1. Research Council of Norway (RCN) through its Centres of Excellence funding scheme [22325]
  2. ARCEx partners
  3. RCN [228107]

向作者/读者索取更多资源

Trough mouth fans comprise the largest sediment deposits along glaciated margins, and record Pleistocene climate changes on a multi-decadal time scale. Here we present a model for the formation of the North Sea Fan derived from detailed horizon and attribute interpretations of high-resolution processed 3D seismic reflection data. The interpretation shows that stacked channel-levee systems form up to 400m thick sedimentary sequences. The channels are elongated and can be traced from the shelf edge towards the deep basin for distances of >150 km, and document long-distance sediment transport in completely disintegrated water-rich turbidite flows. Downslope sediment transport was a continuous process during shelf-edge glaciations, reaching accumulation rates of 100 m/kyr. Our data highlight that exceptionally large volumes of meltwater may discharge to the slopes of trough mouth fans and trigger erosive turbidite flows. We conclude that freshwater supply is likely an underestimated factor for sedimentary processes during glacial cycles.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.8
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

Article Geology

Inside the volcano: Three-dimensional magmatic architecture of a buried shield volcano

Faye Walker, Nick Schofield, John Millett, Dave Jolley, Simon Holford, Sverre Planke, Dougal A. Jerram, Reidun Myklebust

Summary: This study presents the first high-resolution three-dimensional reconstruction of an ancient volcanic plumbing system, revealing a large laccolithic complex formed incrementally through amalgamation of smaller intrusions. Seismic reflection and gravity data show that the complex fed surface volcanism and an extensive sill network, with numerous sills indicating magma stalling at different levels during ascent. This research provides insight into the multicomponent plumbing system within a large ancient shield volcano for the first time.

GEOLOGY (2021)

Article Geography, Physical

Characterization of a glacial paleo-outburst flood using high-resolution 3-D seismic data: Bjornelva River Valley, SW Barents Sea

B. Bellwald, S. Planke, S. Polteau, N. Lebedeva-Ivanova, J. Faleide, S. M. Morris, S. Morse, S. Castelltort

Summary: The study describes the morphology and formation of the Bjornelva River Valley in the SW Barents Sea, suggesting it may represent a braided river system fed by outburst floods from a glacial lake. The valley's configuration could be useful for geohazard assessments in areas at risk of outburst flooding today and as an analogue for landscapes evolving in regions currently covered by ice sheets.

JOURNAL OF GLACIOLOGY (2021)

Article Geography, Physical

The birth and demise of the vast epicontinental Permian Irati-Whitehill sea: Evidence from organic geochemistry, geochronology, and paleogeography

Lucas Pinto Heckert Bastos, Rene Rodrigues, Egberto Pereira, Sergio Bergamaschi, Carmen Lucia Ferreira Alferes, Lars Eivind Augland, Mathew Domeier, Sverre Planke, Henrik Hovland Svensen

Summary: The evolution and demise of the Irati-Whitehill sea can be unraveled through the study of organic geochemical characteristics and tephrochronology, constrained by new high-resolution chemostratigraphic data, the evolution of the sea is divided into five stages.

PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY (2021)

Article Geochemistry & Geophysics

Does Retrogression Always Account for the Large Volume of Submarine Megaslides? Evidence to the Contrary From the Tampen Slide, Offshore Norway

R. S. Barrett, B. Bellwald, P. J. Talling, A. Micallef, F. Gross, C. Berndt, S. Planke, R. Myklebust, S. Krastel

Summary: Submarine landslides can be significantly larger than their terrestrial counterparts and can pose significant hazards across entire ocean basins. The failure mechanism strongly controls the associated tsunami hazard. The Tampen Slide, one of the largest landslides on Earth, was found to have failed mainly as a single volume along a single failure surface, differing significantly from other giant submarine landslides that seem to have failed in multiple phases and involving multiple failure surfaces.

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH (2021)

Article Geography, Physical

Response of macrobenthic trace maker community to the end-Permian mass extinction in Central Spitsbergen, Svalbard

F. J. Rodriguez-Tovar, J. Dorador, V Zuchuat, S. Planke, O. Hammer

Summary: The study focuses on the ichnological analysis of an extended upper Permian - Lower Triassic succession from the DD-1 core, drilled in Deltadalen, Central Spitsbergen. Variations in degree of bioturbation and ichnodiversity across the Permian-Triassic transition allow for the characterization of pre-, syn-, and post-EPME phases.

PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY (2021)

Article Geochemistry & Geophysics

Impacts of seismic resolution on fault interpretation: Insights from seismic modelling

Thea Sveva Faleide, Alvar Braathen, Isabelle Lecomte, Mark Joseph Mulrooney, Ivar Midtkandal, Aina Juell Bugge, Sverre Planke

Summary: Interpreting normal faults faces challenges and pitfalls related to objective and subjective uncertainties. Testing interpretations were classified into 10 scenarios with different fault geometries, utilizing seismic modelling to investigate detailed fault architectures. High-resolution seismic data combined with modelling enhances confidence in conventional seismic interpretation in the same area.

TECTONOPHYSICS (2021)

Article Geochemistry & Geophysics

Seismic Volcanostratigraphy: The Key to Resolving the Jan Mayen Microcontinent and Iceland Plateau Rift Evolution

Anett Blischke, Bryndis Brandsdottir, Martyn S. Stoker, Carmen Gaina, Ogmundur Erlendsson, Christian Tegner, Saemundur A. Halldorsson, Helga M. Helgadottir, Bjarni Gautason, Sverre Planke, Anthony A. P. Koppers, John R. Hopper

Summary: Volcanostratigraphic and igneous province mapping of the Jan Mayen microcontinent and Iceland Plateau Rift region provide new insights into the development of rift systems during breakup processes, revealing two breakup events, seven distinct tectono-magmatic phases, and four rift zones.

GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS (2022)

Article Geosciences, Multidisciplinary

Paleogene drainage system evolution in the NE Faroe-Shetland Basin

Faye Walker, Nick Schofield, John Millett, David Jolley, Sverre Planke, Simon Holford

Summary: Incised drainage systems can record ancient vertical crustal motion. A newly identified incised drainage system in the Faroe-Shetland Basin formed during a period of rapid uplift about 56 million years ago. This erosional surface is a composite feature, influenced by igneous intrusions, and records prolonged regional uplift.

JOURNAL OF THE GEOLOGICAL SOCIETY (2022)

Article Geosciences, Multidisciplinary

Characterizing ancient and modern hydrothermal venting systems

Ben Manton, Philipp Muller, Adriano Mazzini, Dmitry Zastrozhnov, Dougal A. Jerram, John M. Millett, Daniel W. Schmid, Christian Berndt, Reidun Myklebust, Sverre Planke

Summary: Ancient and modern hydrothermal venting systems are related, as evidenced by the morphological similarities between the offshore mid-Norway vent complex and the Java venting system. Both systems are formed through the transport and eruption of fluidized sediments.

MARINE GEOLOGY (2022)

Article Geosciences, Multidisciplinary

Tectonostratigraphic development of the Upper Triassic to Middle Jurassic in the Hoop Area, Barents Sea: Implications for understanding ultra-condensed reservoir units

R. Muller, T. G. Klausen, L. H. Line, A. Hafeez, S. Planke, F. Eide, E. Stueland, J. Jahren, B. Rismyhr, S. Olaussen

Summary: This study focuses on the tectono-stratigraphic evolution of the Realgrunnen Subgroup in the Barents Sea, identifying seven major phases of deposition and non-deposition/erosion. The results are crucial for exploration and production in the Hoop Area and provide insights into the evolution of ultra-condensed successions during periods of non-deposition.

MARINE AND PETROLEUM GEOLOGY (2022)

Article Geosciences, Multidisciplinary

Characterization of volcanic reservoirs; insights from the Badejo and Linguado oil field, Campos Basin, Brazil

Gabriel M. Marins, Yaro Parizek-Silva, John M. Millett, Dougal A. Jerram, Lucas M. M. Rossetti, Ariany de Jesus e Souza, Sverre Planke, Leandro A. Bevilaqua, Isabela de O. Carmo

Summary: This study provides a comprehensive evaluation of volcanic reservoirs in offshore oil fields in Brazil, revealing the key role of primary volcanic facies and subsequent alteration history in determining reservoir properties.

MARINE AND PETROLEUM GEOLOGY (2022)

Article Geosciences, Multidisciplinary

The interplay between siliciclastic and carbonate depositional systems: Maastrichtian to Danian basin-floor sediments of the mid-Norwegian More Basin

Hans Jorgen Kjoll, Ivar Midtkandal, Sverre Planke, John Millett, Ben Manton, Kresten Anderskouv

Summary: This study describes and deciphers a late Maastrichtian to Danian-aged basin-floor depositional system in the deep outer More Basin, mid-Norwegian margin. The study integrates and utilizes wireline geophysical logs, detailed petrographic observations from side-wall cores, and seismic analysis. The research provides insights into sediment transport, provenance, and depositional processes in a pre-breakup source-to-sink sedimentary system near an infant ocean's breakup axis.

BASIN RESEARCH (2023)

Article Geosciences, Multidisciplinary

Shallow-water hydrothermal venting linked to the Palaeocene-Eocene Thermal Maximum

Christian Berndt, Sverre Planke, Carlos A. Alvarez A. Zarikian, Joost Frieling, Morgan T. T. Jones, John M. M. Millett, Henk Brinkhuis, Stefan Bunz, Henrik H. H. Svensen, Jack Longman, Reed P. P. Scherer, Jens Karstens, Ben Manton, Mei Nelissen, Brandon Reed, Jan Inge Faleide, Ritske S. S. Huismans, Amar Agarwal, Graham D. M. Andrews, Peter Betlem, Joyeeta Bhattacharya, Sayantani Chatterjee, Marialena Christopoulou, Vincent J. J. Clementi, Eric C. C. Ferre, Irina Y. Y. Filina, Pengyuan Guo, Dustin T. T. Harper, Sarah Lambart, Geoffroy Mohn, Reina Nakaoka, Christian Tegner, Natalia Varela, Mengyuan Wang, Weimu Xu, Stacy L. L. Yager

Summary: Widespread shallow-water hydrothermal venting in the North Atlantic, probably a source of methane, coincided with the onset of the Palaeocene-Eocene Thermal Maximum. This venting occurred around 56 million years ago and was caused by carbon input into the ocean and atmosphere, leading to a global warming event. The vents erupted in shallow water, resulting in the direct release of volatile emissions without oxidation to CO2, and played a key role in the carbon-cycle perturbation.

NATURE GEOSCIENCE (2023)

Article Geology

Holocene seismic activity in south-eastern Switzerland: Evidence from the sedimentary record of Lake Silvaplana

Benjamin Bellwald, Valentin Nigg, Stefano C. Fabbri, Lukas W. M. Becker, Adrian Gilli, Flavio S. Anselmetti

Summary: This study aims to evaluate the paleoseismic activity in southeastern Switzerland by analyzing the sedimentary record of Lake Silvaplana. The analysis of acoustic exploration data from the lake floor reveals that four large landslide events have occurred in the last 1400 years, which is consistent with sediment records from other lakes. This provides a reliable record of seismic activity during the mid and Late Holocene in the region, likely related to the neotectonic activity of the Engadine Line.

SEDIMENTOLOGY (2023)

Article Geosciences, Multidisciplinary

Tracing North Atlantic volcanism and seaway connectivity across thePaleocene-Eocene Thermal Maximum (PETM)

Morgan T. Jones, Ella W. Stokke, Alan D. Rooney, Joost Frieling, Philip A. E. Pogge von Strandmann, David J. Wilson, Henrik H. Svensen, Sverre Planke, Thierry Adatte, Nicolas Thibault, Madeleine L. Vickers, Tamsin A. Mather, Christian Tegner, Valentin Zuchuat, Bo P. Schultz

Summary: There is a temporal correlation between the peak activity of the North Atlantic Igneous Province (NAIP) and the Paleocene-Eocene Thermal Maximum (PETM), suggesting that the NAIP may have initiated and/or prolonged this extreme warming event. However, corroborating a causal relationship is hampered by a scarcity of expanded sedimentary records that contain both climatic and volcanic proxies.

CLIMATE OF THE PAST (2023)

暂无数据