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Marine Geology
Elsevier Science B.V.
Marine Geology

Elsevier Science B.V.

0025-3227

Marine Geology/Journal Marine GeologySCIISTPAHCIEI
正式出版
收录年代

    Shallow gas and gas hydrate occurrences on the northwest Greenland shelf margin

    Cox, David R.Huuse, MadsNewton, Andrew M. W.Sarkar, Arka D....
    21页
    查看更多>>摘要:An extensive 3D seismic dataset was used to investigate the contemporary hydrocarbon distribution and historical fluid migration in Melville Bay offshore northwest Greenland, providing the first inventory of shallow gas and gas hydrate along this part of the Greenland margin. The shallow gas anomalies vary in seismic character and have been subdivided into four categories that represent (I) isolated shallow gas, (II) free gas trapped at the base of the gas hydrate stability zone (GHSZ), (III) gas charged glacial clinoforms and (IV) a giant mass transport deposit gas reservoir. Gas hydrate deposits have been identified across an area of 537 km(2) via the identification of a discontinuous bottom simulating reflector (B SR) that marks the base of the GHSZ. The BSR has been used to estimate a geothermal gradient of 49 degrees C/km across the GHSZ and a heat flow of 70-90 mW/m(2) , providing the first publically available heat flow estimates offshore western Greenland. The contemporary hydrocarbon distribution and historical fluid migration is influenced by the underlying paleo-rift topography and multiple shelf edge glaciations since -2.7 Ma. Continued uplift of the Melville Bay Ridge, as well as glacial-sediment redistribution and basinward margin tilting from isostatic compensation, have led to a concentration of gas within the Cenozoic stratigraphy above the ridge. Furthermore, repeated variations in subsurface conditions during glacial-interglacial cycles likely promoted fluid remigration, and possibly contributed to reservoir leakage and increased fluid migration through faults. The top of the gas hydrate occurrence at 650 m water depth is well below the hydrate-free gas phase boundary (-350 m) for the present bottom-water temperature of 1.5 degrees C, suggesting this hydrate province mainly adjusted to glacial-interglacial changes by expansion and dissociation at its base and is relatively inert to current levels of global warming. Glacial-related dissociation may have significantly contributed to the numerous free gas accumulations observed below the GHSZ at present day.

    Submarine morphology of the Comoros volcanic archipelago

    Tzevahirtzian, A.Zaragosi, S.Bachelery, P.Biscara, L....
    23页
    查看更多>>摘要:A detailed morpho-bathymetric study of the Comoros archipelago, based on mostly unpublished bathymetric data, provides a first glimpse into the submarine section of these islands. It offers a complete view of the distribution of volcanic structures around the archipelago, allowing to discuss the origin and evolution of this volcanism. Numerous volcanic cones and erosional-depositional features have been recognized throughout the archipelago. The magmatic supply is focused below one or several volcanoes for each island, but is also controlled by lithospheric fractures evidenced by volcanic ridges, oriented along the supposed Lwandle-Somali plate boundary. Massive mass-wasting morphologies also mark the submarine flanks of each island. Finally, the submarine geomorphological analysis made possible to propose a new scheme for the succession of the island's growth, diverging from the east-west evolution previously described in the literature.

    Deep learning model for seabed sediment classification based on fuzzy ranking feature optimization

    Cui, XiaodongYang, FanlinWang, XinAi, Bo...
    14页
    查看更多>>摘要:Accurate acquisition of information on seabed sediment distributions plays an important role in the construction of basic marine geographic databases. Although a multibeam echo-sounding system (MBES) can satisfy large-scale seafloor mapping with high precision and high resolution, the development of a consistent, stable, repeatable and validated seabed sediment classification method based on swath acoustic data is still in its infancy. To achieve accurate prediction and mapping of geographic seabed sediment information, this paper developed a deep learning model based on feature optimization. First, faced with high-dimensional features extracted from multibeam bathymetry and backscatter intensity measurement data, a fuzzy ranking (FR) feature optimization method was proposed. By combining the physical properties of actual sediment samples, the multidimensional features derived from terrain and intensity data are ranked and optimally selected according to the mean square error to eliminate redundant and irrelevant features. Second, the deep belief network (DBN) deep learning method was used to build a supervised seabed sediment classification model. The optimized features and actual sediment samples participate in model training, which further enhances the prediction ability of acoustic data to seabed sediments. Finally, to evaluate the performance of the DBN model, this experiment used large-scale multibeam survey data and ground-truth data (acquired by grabbers, core samplers, dredges, etc.) in the southern Irish Sea to achieve accurate prediction of 10 sediment types (slightly gravelly muddy sand, slightly gravelly sand, gravelly mud, gravelly muddy sand, gravelly sand, muddy sand, muddy sandy gravel, sand, sandy gravel and sandy mud). The experiment results show that by using the optimal feature combination based on FR, the overall classification accuracy and Kappa coefficient reached 86.20% and 0.834, respectively, which are significantly improved compared to the evaluation metrics of other feature selection methods. In addition, compared with the current five typical supervised classification methods (i.e., the random forests, BP neural network, support vector machine, maximum likelihood and decision trees methods), the proposed DBN classification model achieves a better performance, highlighting its application potential in seabed sediment detection and mapping.

    Paleoenvironmental implications of Sr and Nd isotopes variability over the past 48 ka from the southern Sea of Japan

    Zou, JianjunShi, XuefaZhu, AimeiHe, Lianhua...
    14页
    查看更多>>摘要:Millennial scale variations of terrigenous provenance in marine realm are closely related to regional environment and climate changes. Therefore, a wealth of information of past environment and climate can be constrained via fingerprinting sediment provenance. The Sea of Japan is a unique marginal sea in the North Pacific due to its high sill and distinct thermohaline circulation. The modern hydrography in the Sea of Japan is mainly affected by the East Asian Monsoon and Tsushima Warm Current, one branch of the Kuroshio Current. The Sea of Japan communicates with neighboring seas through four shallow and narrow straits, indicating great effects of global eustatic sea level change on its environment over glacial-interglacial cycles. Here we examine the terrigenous provenance in fine-grained fraction (<63 mu m) of core KCES1, located near one end of the Tsushima Strait of the Sea of Japan over the last 48 ka, using radiogenic isotopes of strontium (Sr) and neodymium (Nd). Our data suggest that the terrigenous provenance in core KCES1 was mainly derived from the Yangtze River after 7 ka and a mixture of Yangtze and Yellow Rivers during the last glacial and deglacial periods. Notably, pronounced negative excursions of epsilon Nd values at HS1 were attributed to minor additions of unradiogenic Nd contribution from China-Korea cratonic hinterland. A binary mixing model further reveals that >85% terrigenous material is derived from the Yangtze and Yellow Rivers over the last 48 ka. Moreover, abrupt variations in sediment provenance occurred at similar to 18 ka and similar to 7 ka, which coincide with variations in oceanic surface circulation and deep ventilation recorded in the Sea of Japan. We suggest that paleo-Tsushima Warm Current invaded into the Sea of Japan with reopening of the Tsushima Strait at HS1 and the Tsushima Warm Current substantially entered the Sea of Japan after 7 ka due to intensified Kuroshio Current and rising eustatic sea level. The inflow of Tsushima Warm Current gives rise to a range of changes in surface hydrography, deep ventilation, ecological communities and productivity and sediment texture. The combination of fluxes of paleo-rivers and the intensity of Kuroshio Current, which are closely tied to the eustatic sea level and the East Asian Monsoon, plays a key role in controlling the variations in sediment provenance in the Ulleung Basin. Our study provides unique insight into the tight coupling between changes in sediment provenance and oceanic environment over the last 48 ka in the Sea of Japan.

    Embayment morphometrics, granulometry and carbonate mineralogy of sandy beaches in the Maltese Islands

    Gatt, Peter
    14页
    查看更多>>摘要:The beach and shoreface sediments in the Maltese Islands have accumulated in under-filled accommodation space conditions like many temperate and tropical island carbonate beach and shelf environments. Nevertheless, Maltese beach sediments show anomalously low biogenic carbonate content compared to other carbonate beaches. Fourteen carbonate sandy beaches in the Maltese Islands were sampled to examine the relationships between geological controls on both coastal lithology and configurations of bays and beaches and, grain characteristics described by granulometry and mineralogy. The provenance of the medium to coarse-grained beach sand is mainly from the erosion of coastal and shelf Cenozoic limestone that produces lithoclasts of low-magnesium calcite, with an additional 20 +/- 10% biogenic grains derived from marine carbonate productivity. The relationships between geological controls and beach sediments are used to establish a general model of sedimentation along the Maltese shelf area. Mean beach sand size is controlled by the degree of embayment, decreasing where bays are narrower and longer, whereas sediment provenance affects granulometry by the contribution of biogenic grains to the coarse and fine grain size fractions. The mineralogy of the biogenic sediment fraction in beaches is mainly high-magnesium calcite and aragonite, with the latter decreasing significantly where coastal clay is found within or close to bays.

    A diatom-based Holocene record of sedimentary and oceanographic environmental changes within the Beibu Gulf, NW South China Sea

    Zhang, JinpengTomczak, MichalWitkowski, AndrzejLiang, Kai...
    13页
    查看更多>>摘要:A sediment core from a nearshore setting (10.8 m in water depth) of the inner Beibu Gulf, northwestern South China Sea, was analyzed in terms of diatom assemblage composition, grain size distribution and radiocarbon dating, with aim to describe sedimentary and oceanographic environmental changes during the Holocene. The fossil diatom record and changes in granulometry reveal that sea-level fluctuations had a strong influence on the evolution of hydrographic system, which changed significantly with rapid sea-level rise in the early Holocene ca. 10,000-7800 cal. yr. BP. These fluctuations continued in a series of stages dated to the middle Holocene ca. 7800-6200 cal. yr. BP, with sea-level increase, followed by a prolonged sea-level retreat during ca. 6200 to 3300 cal. yr. BP, and finally a relatively high sea level from ca. 3300 cal. yr. BP to the present. The resultant sedimentary facies could be divided into seven stages inferred by the diatom distribution and grain size characteristics: a river channel/beach environment at ca. 10000-9500 cal. yr. BP, a lagoonal environment at ca. 9500-7800 cal. yr. BP, a relatively broad embayment at ca. 7800-6200 cal. yr. BP, a bay at ca. 6200-3300 cal. yr. BP and a coastal environment setting up to present day. The coastal environmental setting has been subject to some shifts in climate and sea-level beginning with strong terrestrial influx at ca. 3300-1400 cal. yr. BP, which was then replaced by strong hydrological circulation at ca. 1400-800 cal. yr. BP, and a relative stable sedimentary environment approximate to the coast from ca. 800 cal. yr. BP to present.

    High-resolution depositional records of lead isotopes and polycyclic aromatic hydrocarbons in the Bohai Sea, China: Implications for a sediment footprint of anthropogenic impact

    Wu, BinLiu, JianGuo, ZhigangChen, Bin...
    10页
    查看更多>>摘要:Mercury (Hg), Lead (Pb) and its stable isotopes and polycyclic aromatic hydrocarbons (PAHs) were analyzed in a sediment box core obtained from the central Bohai Sea (BS) of northern China to trace anthropogenic input for the past century. The records of Hg, PAHs and Pb isotopic ratios revealed that the BS was clearly impacted by human activities from the early 1930s to the middle 1940s, possibly related to the acceleration of heavy industrialization in northeast China. Under rapid development and significant increase in fossil fuel consumption, pressure on the BS environment had obviously increased, as revealed by increasing concentrations of Hg, Pb, and PAHs from the early 1960s to late 1990s, with a synchronous decrease of Pb-206/Pb-207 isotopic ratios. The evolving trends in Pb-206/Pb-207 ratio, Hg, and PAHs were found to be decoupled since the early 2000s, possibly because of the significant improvement in environmental protection. Depositional records of Pb isotopic ratios with PAH compositions indicate a high-resolution sediment footprint of anthropogenic energy-consumption-based impacts around the BS over the past century, especially with the transformed emission sources from the leaded gasoline and combustion of coal before the 2000s to coal combustion and nonferrous metal smelting thereafter. The decreased records of sedimentary Pb have been widely found by around the world (e.g. North America, Southeast Asia and West Europe) after the ban on the leaded gasoline. However, this trend in China is reverse by the phasing out of leaded gasoline since the 2000s, possibly due to the recent accelerating development of nonferrous metal smelting and the continued increase in coal-dominated energy consumption.

    Relative sea-level stability and the radiocarbon marine reservoir correction at Natuna Island, Indonesia, since 6400 yr BP (vol 430, 106342, 2020)

    Wan, Jeannette Xiu WenMeltzner, Aron J.Switzer, Adam D.Lin, Ke...
    2页

    Modelling flocculation: Towards an integration in large-scale sediment transport models (vol 430, 106361, 2020)

    Chassagne, C.Safar, Z.
    1页

    Inter-comparison of optically stimulated luminescence (OSL) ages between different fractions of Holocene deposits from the Yangtze delta and its environmental implications

    Nian, XiaomeiZhang, WeiguoWang, ZhanghuaSun, Qianli...
    10页
    查看更多>>摘要:In fluvial and deltaic environments, different grain-size fractions experience varying degrees of bleaching of OSL signals due to variations in hydrodynamics and depositional processes. This has led to ambiguity for selection of grain-size fraction suitable for OSL dating. Comparison of OSL results from multiple grain-size fractions is one approach to ensure the reliability of OSL ages. We determined the quartz OSL ages of four grain-size fractions from fine silt to sand, together with the single grain OSL sensitivity in a Holocene sediment core from the Yangtze delta. For samples from the lower part of the sediment succession (including tidal river, tidal trough fill, estuarine front, tidal sand and delta front facies), OSL ages determined for different grain-size fractions were generally mutually consistent within the age range of similar to 2-9 ka, implying minor portion of incompletely bleached grains in the sediment at the time of burial. In contrast, significant partial bleaching was observed for three samples from younger delta front facies deposited during 0.4-0.6 ka. In these three samples, fine-silt quartz OSL ages were overestimated by similar to 0.5-2.0 ka compared with ages of coarser fractions. Based on the investigation of quartz luminescence sensitivity, we suggest that the southward shift of the Yellow River and increasing erosion in the Yangtze River catchment have led to enhanced water turbidity, resulting in partial bleaching of the sediment and substantial overestimation of the quartz OSL ages of fine silt during 0.4-0.6 ka. Alternatively, the erosion of older deposits and their redeposition elsewhere could retain large residual OSL ages. Notably, fine-silt quartz provides reliable ages for the period of 9-2 ka, suggesting that there was a lower degree of water turbidity compared with that since 2 ka. Therefore, the degree of OSL age overestimation may provide an indication of changes in water turbidity and sedimentary environment. Overall, our findings highlight the complexity of OSL dating in delta environments, and that an understanding of sediment transport and depositional processes is critical for reliable OSL dating.