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  • 1. Andrén, Thomas
    Baltic Sea Science Congress 2001 - Preface2005In: Quaternary International, ISSN 1040-6182, E-ISSN 1873-4553, Vol. 130, no 1Article in journal (Refereed)
  • 2. Andrén, Thomas
    et al.
    Brunnberg, L
    Miller, U
    PROCEEDINGS FROM THE BALTIC-ICE-LAKE-YOLDIA-SEA-SYMPOSIUM, MARCH 1993: PREFACE1995In: Quaternary International, ISSN 1040-6182, E-ISSN 1873-4553, Vol. 27, p. 3-3Article in journal (Other academic)
  • 3. Andrén, Thomas
    et al.
    Sohlenius, Gustav
    Late Quaternary development of the north-western Baltic Proper: Results from the clay-varve investigation1995In: Quaternary International, ISSN 1040-6182, E-ISSN 1873-4553, Vol. 27, p. 5-10Article in journal (Refereed)
    Abstract [en]

    Within the project "Late Quaternary development of the north-western Baltic Proper" a total of 36 piston core samples have been collected. The results presented in this study are based on analyses of 7 cores with emphasis on the late glacial part of the sequence. The varved glacial clay sequences have been analyzed for calcareous micro-fossils and mineral magnetic properties as well as measurements of clay-varves. The results from these analyses indicate that there is a close correlation between the occurrence of brackish water ostracods and foraminifera and a distinct change in the mineral magnetic parameters. The lithological composition of the clay-varves also differs in this sequence. The duration of this marine phase of the Yoldia Sea stage is 60 to 120 clay-varve years. It is concluded that correlations between the cores can be made using fossil assemblages and mineral magnetic parameters. It has not yet been possible, however, to make any reliable clay-varve connections.

  • 4. Wastegård, S
    et al.
    Andrén, Thomas
    Sohlenius, G
    Sandgren, P
    Different phases of the Yoldia Sea in the north-western Baltic Proper1995In: Quaternary International, ISSN 1040-6182, E-ISSN 1873-4553, Vol. 27, p. 121-129Article in journal (Refereed)
    Abstract [en]

    Four sediment cores from the north-western Baltic Proper, covering the time from the Weichselian deglaciation to the present have been studied. Main interest is focused on the Yoldia stage, and especially the duration of the marine phase of this stage. The lithological compositions of the sediments and results of different analyses (magnetic, carbonate, ostracods and foraminifera) have resulted in a subdivision into five stratigraphical units (A-E, from older to younger). Unit A was deposited in a glaciolacustrine environment, probably during the first non-saline phase of the Yoldia stage. The first ingression of saline water is recorded in unit B. Brackish water ostracods and foraminifera occur exclusively in this unit, which represents the only saline phase of the Yoldia stage. This phase lasted for less than 120 clay varve years. Unit C was deposited in fresh water, probably during the last phase of the Yoldia stage and the Ancylus stage. The uppermost units, D and E are of Holocene age and represent different phases of the Litorina and Post-Litorina stages.

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