Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Lemke, Wolfram; Endler, Rudolf; Tauber, Franz; Jensen, Jorn Bo; Bennike, Ole (1998): (Table 1) Radiocarbon ages of core AB01/94 obtained in the Tromper Wiek, western Baltic Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.785499, Supplement to: Lemke, W et al. (1998): Late- and postglacial sedimentation in the Tromper Wiek northeast of Rügen (western Baltic). Meyniana, 50, 155-173, https://doi.org/10.2312/meyniana.1998.50.155

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
In the Tromper Wiek northeast of Rügen, acoustical investigations using Air Gun, Boomer, Chirp Sonar and Sediment-Echosounder were carried out. Together with sediment core information, it allowed the identification of five seismostratigraphic units (E1 to E5). Conventional and AMS-14C-datings supported their chronostratigraphical classification. The uppermost till (E1) was incised by late glacial channels filled with glaciolacustrine sediments (E2) of the early Baltic Ice Lake stages. These were regionally overlain with a sharp unconformity by a thick (locally >20 m) sedimentary complex (E3) of acoustically laminated silts of freshwater origin. This lower part of the E3-complex (E3a) is overlain by fluvial to coastal silty fine sands (E3b) deeper towards the Arkona Basin. Fine plant debris in the uppermost part of sub-unit E3a yielded ages of 10,100 and 10,500 14C-years B.P., representing the final phase of the Baltic Ice Lake. The fine sands of sub-unit E3b were deposited after the final drainage of the Baltic Ice Lake.
In the shallower central part of the bay, the silts of sub-unit E3a were covered by a younger unit (E4) of fine sand with plant debris. A sedge peat occurring at the basis of unit E4 yielded an age of 9,590 14C-years B.P. The fine sands overlying the unit E3 in the central part of Tromper Wiek were deposited in the Ancylus Lake. Their position at about 20 m below present sea level (b.s.l.) reflects the maximum highstand in this area. The character and distribution of the Early Holocene deposits at greater depth suggest a lake water level at about 30 m b.s.l. after this highstand. Below 25 m b.s.l. muddy Littorina Sea sediments are observed. The thickness of these muds and sandy muds increases gradually towards the Arkona Basin. Locally, they are found in a channel-like structure immediately north of Jasmund.
Coverage:
Latitude: 54.638160 * Longitude: 13.479500
Minimum DEPTH, sediment/rock: 1.7125 m * Maximum DEPTH, sediment/rock: 5.7000 m
Event(s):
AB01/94 * Latitude: 54.638160 * Longitude: 13.479500 * Elevation Start: -21.4 m * Elevation End: -27.2 m * Location: Arkona Basin * Method/Device: Vibro corer (VC)
Comment:
Calibration according to calibration tables in the journal Radiocarbon, vol. 35, 1993.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample IDSample IDLemke, Wolfram
CoreCoreLemke, Wolfram
Depth, top/minDepth topmLemke, Wolfram
Depth, bottom/maxDepth botmLemke, Wolfram
DEPTH, sediment/rockDepth sedmGeocode
Sample typeSamp typeLemke, Wolfram
Age, datedAge datedka BPLemke, WolframAge, 14C AMSka BP
Age, dated standard deviationAge dated std dev±Lemke, WolframAge, 14C AMS
Calendar ageCal ageka BPLemke, WolframAge, 14C calibrated
10 Calendar age, standard deviationCal age std dev±Lemke, WolframAge, 14C calibrated1 stdv.
11 δ13Cδ13C‰ PDBLemke, Wolfram
Size:
30 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sample ID

Core

Depth top [m]

Depth bot [m]

Depth sed [m]

Samp type

Age dated [ka BP]

Age dated std dev [±]

Cal age [ka BP]
10 
Cal age std dev [±]
11 
δ13C [‰ PDB]
K-6339AB 01/941.6751.751.7125Sedge peat9.590.1410.4210.96-28.6
AAR-1921AB 01/941.8702.001.9350Plant rootlets10.100.1211.0812.04-25.0
AAR-1920 rootletsAB 01/945.6005.805.7000Plant rootlets10.570.1512.3112.66-25.0