Site M0060

Andrén, Thomas; Jørgensen, B.B.; Cotterill, C.; Green, S.; Andrén, Elinor; Ash, Jeanine L.; Bauersachs, Thorsten; Cragg, Barry A.; Fanget, A.-S.; Fehr, A.; Granoszewski, Wojciech; Groeneveld, Jeroen; Herrero‐Bervera, Emilio; Hyttinen, Outi; Jensen, J.B.; Johnson, Sean; Kenzler, Michael; Kotilainen, Aarno; Kotthoff, Ulrich; Marshall, I.P.G.; Martin, E.; Obrochta, Stephen; Passchier, Sandra; Krupinski, N. Quintana; Riedinger, Natascha; Slomp, Caroline P.; Snowball, Ian; Stepanova, A.; Strano, S.; Torti, A.; Warnock, Jonathan P.; Xiao, Nan; Zhang, R.

doi:10.2204/iodp.proc.347.104.2015

Cited by 3 publications

(15 citation statements)

References 14 publications

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“…), and drilled at IODP site M 0060 in 2012 (Andrén et al . ). We assume drainage systems related to the recent large Oder and Vistula rivers crossing our study area (Fig.…”

Section: Discussionmentioning

confidence: 97%

The Late Saalian Cyprina clay of northeastern Germany and the following Weichselian sedimentation and deformation history – Review and new data

Obst

Ansorge

Thiel

et al. 2020

Boreas

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Glacially dislocated fossiliferous clay – hitherto called Cyprina clay– and associated Pleistocene sediments are exposed at the northeastern German coast. They were uplifted as glacial rafts from a position of about 30 m below the sea level and incorporated into glaciotectonic complexes of Dornbusch (Hiddensee), Arkona (Rügen) and Greifswalder Oie during the ice advances of the Last Glacial Maximum (LGM). Optically stimulated luminescence (OSL) ages of the fossil‐bearing clay and the overlying glacifluvial/lacustrine successions give insights into Late Saalian, Eemian and Early to Middle Weichselian development of the southern Baltic Sea area. The age data especially support the observation of changing environmental conditions prior to the Eemian warm period as suggested by the fossil record. A high‐arctic brackish fauna documented in a lower reddish‐grey clay is followed by a more boreal brackish‐marine to marine fauna in the overlying olive and/or greenish‐grey clay. This implies conditions of glacial meltwater running to the northwest during the deglaciation phase of the last Saalian Warthe ice advance and inflow of cold marine water from the North Atlantic area along the margin of the Scandinavian Ice Sheet into the Skagerrak and the Kattegat. Subsequently, water with higher salinity entered the mouths and channels of large rivers crossing the southern Baltic Sea area from SE to NW comparable with those of the Oder and Vistula rivers. Eemian Cyprina clay deposits with lusitanian faunal elements are not exposed in the study area but occur in Denmark and northwestern Germany. To distinguish the different facies types and age of the clay, we introduce the stratigraphical term Vitt Formation for the Late Saalian Cyprina clay in NE Germany, comprising Roundstonia, Portlandia and Arctica members – each with characteristic microfossil species.

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“…), and drilled at IODP site M 0060 in 2012 (Andrén et al . ). We assume drainage systems related to the recent large Oder and Vistula rivers crossing our study area (Fig.…”

Section: Discussionmentioning

confidence: 97%

The Late Saalian Cyprina clay of northeastern Germany and the following Weichselian sedimentation and deformation history – Review and new data

Obst

Ansorge

Thiel

et al. 2020

Boreas

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show abstract

“…Coarse sand (Briggs 1994) Fine sand 1 (Briggs 1994) Fine sand 2 (Briggs 1994) Coarse sand (Jackson et al 1996) Sand (Goldhammer 1997) Sand (Taylor et al 1999) Sand (Inagaki et al 2003) Sand (Fisher et al 2005) Sand 1 (Ferdelman et al 2006) Sand 2 (Ferdelman et al 2006) Sand (Kominz et al 2011) Sand (Takai et al 2011) Sand (Andrén et al 2015b) Silt 1 (Briggs 1994) Silt 2 (Briggs 1994) Silt (Jackson et al 1996) Silt (Goldhammer 1997) Silt 1 (Carter et al 1999) Silt 2 (Carter et al 1999) Silt 3 (Carter et al 1999) Silt (Moore et al 2001b) Clay (Richardson & Briggs 1993) Clay (Goldhammer 1997 minutes after each insertion, as soon as any excess pore-water pressure dissipates).…”

Section: Test Proceduresmentioning

confidence: 99%

Depth-Dependent Seabed Properties: Geoacoustic Assessment

Lyu

Park

Santamarina

2021

J. Geotech. Geoenviron. Eng.

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“…For this purpose, sediment cores have been retrieved from different settings in the Baltic Sea covering the last glacial-interglacial cycle (Andrén et al, 2015a). Site M0060, the focus of this study, was drilled close to Anholt Island, located in the Kattegat region of the Baltic Sea (Andrén et al, 2015b).…”

Section: Introductionmentioning

confidence: 99%

“…Because of relatively high sedimentation rates since the last glacial cycle, the Anholt Basin contains a high-resolution IODP Proceedings 2 V o l u m e 3 4 7 sediment sequence (Andrén et al, 2015a). Site M0060 is characterized by mass transported, unsorted to poorly sorted diamict Lithostratigraphic Unit VII in the lowermost part of the core (Andrén et al, 2015b). On top of this unit, alternating sandy and silty sequences dominate (Units VI-I), and varved glacial clays (Units III-II) indicate deposition in a glacial lake or marginal marine environment.…”

Section: Introductionmentioning

confidence: 99%

“…On top of this unit, alternating sandy and silty sequences dominate (Units VI-I), and varved glacial clays (Units III-II) indicate deposition in a glacial lake or marginal marine environment. Based on pore water chloride data, sand-dominated Units IV and VI indicate freshwater influence (Andrén et al, 2015b). Solid-phase major and minor element contents can be used to characterize sediment sequences that accumulated in the Anholt Basin during various depositional environments throughout the last interglacial-glacial cycle (Andrén et al, 2015b).…”

Section: Introductionmentioning

confidence: 99%

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