Palaeoclimatic changes in Kveithola, Svalbard, during the Late Pleistocene deglaciation and Holocene: Evidences from microfossil and sedimentary records. Palaeogeogr. Palaeoclimatol. Palaeoecol. 2016, 463, 136-149. [CrossRef]Carbonara, K., Mezgec, K., Varagona, G., Musco, M. E., Lucchi, R....
您可以在这个前采矿小镇漫步,该小镇的教区教堂和斯瓦尔巴特博物馆(Svalbard Museum)为您提供迷人的景点。虽然农村看似鲜明,但已有超过一百种植物被记录在其中。在傍晚,船驶出Isfjorden,在那里你可以发现你的第一头小须鲸。You touch down in Longyearbyen, the administrative center of Spitsbergen, the largest island...
Distribution of modern benthic foraminifera from fjords of Svalbard, European Arctic J. Foramin. Res., 27 (1997), pp. 101-122 CrossrefView in ScopusGoogle Scholar Hanebuth et al., 2000 T. Hanebuth, K. Stattegger, P.M. Grootes Rapid flooding of the Sunda Shelf: a Late-Glacial sea-...
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This study reports diverse spiriferellid brachiopods from the Permian rocks of Svalbard and adjacent areas (Arctic Canada and Subpolar Urals of Russia) loc... S Lee,GR Shi,J Woo,... - 《Journal of Systematic Palaeontology》 被引量: 0发表: 2019年 ...
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Conversely, the late Holocene was governed by deteriorating climatic conditions, with predominant Arctic/Polar water inflow on the surface water masses off Western Svalbard, possibly associated with summer insolation decline due to orbital forcingKatia...
The volume of the Kvitoya TMF is smaller than TMFs along the western Svalbard margin, which may be linked to the more erosion-resistant bedrock of the northern margin and/or the comparatively small drainage basin of Kvitoya Trough compared to drainage basins of ice streams that drained ...
World‐class examples of fault‐controlled growth basins with associated syn‐kinematic sedimentary fill are developed in Upper Triassic prodelta to delta‐front deposits exposed at Kvalpynten, SW Edgeya in East Svalbard. They are interpreted to have interacted with north‐westerly progradation of a...