{"refrec":{"BRefID":15848,"RR":"<b>van Weering, T.C.E.; Berger, G.W.; Kalf, J.</b> (1987). Recent sediment accumulation in the Skagerrak, Northeastern North Sea. <i>Neth. J. Sea Res. 21(3)</i>: 177-189","BEntID":15848,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Neth. J. Sea Res. 21(3)</i>: 177-189","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van Weering, T.C.E.; Berger, G.W.; Kalf, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van Weering, T.C.E. <i>et al.</i>","Englishabstract":"Recent sedimentation and sediment accumulation rates calculated from downcore <sup>210</sup>Pb excess activity profiles in 16 boxcores from the Skagerrak show great variations. Highest sedimentation rates, in excess of 0.40 cm·y<sup>-1</sup>, are found in the northeastern Skagerrak. Intermediate values (~0.20 cm·y<sup>-1</sup>) occur both along the southern and northern slopes of the basin. The central basin is characterized by values of ~0.10 cm·y<sup>-1</sup>. These sedimentation rates evidence that 28.4 million tons (dry weight) of sediment accumulate annually in the Skagerrak, of which some 59% (16.7 million tons) are finer than 63 µm. The organic carbon content of the bottom sediments is 2.5% of dry weight in the deepest part of the basin where the finest sediment settles, around 2% in the northern and eastern sectors and on average around 1.5% in the southern part of the study area. Downcore deviations from the logarithmic decrease of <sup>210</sup>Pb with depth could generally be attributed to biologial disturbance causing reworking of the sediment, as shown by ETS measurements and X-radiography. The Skagerrak is evidently the major depository of fine-grained sediments in the North Sea. The role of sea-floor erosion as an additional source of sediment has most probably been highly underestimated in mass budget studies so far.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Recent sediment accumulation in the Skagerrak, Northeastern North Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1987,"MonPub":null,"DateUpdate":"2019-07-10","DateCreate":"2001-08-17","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1987K642800003","VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":15848,"PubliDate":1987,"Pagination":"177-189","XtraPublOfAnaID":null,"ISBN":null,"Volume":"21","Issue":"3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":44573,"SerRR":"Netherlands Journal of Sea Research. 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