Main environmental changes since the Weichselian glaciation in the Danish waters between the North Sea and the Baltic Sea as reflected in the molluscan fauna

K.S. Petersen; K.L. Rasmussen; Peter Rasmussen; Frants von Platen-Hallermund

doi:10.1016/j.quaint.2004.10.013

Main environmental changes since the Weichselian glaciation in the Danish waters between the North Sea and the Baltic Sea as reflected in the molluscan fauna

K.S. Petersen
, K.L. Rasmussen
, Peter Rasmussen
, Frants von Platen-Hallermund

Research output: Contribution to journal › Article › Research › peer-review

17 Citations (Scopus)

Abstract

The Danish waters forming the transition zone between the North Sea and the Baltic Sea are described through changes in the molluscan fauna and bottom communities during the Holocene. The major change in the fauna at the Pleistocene-Holocene boundary is thought to be caused by changes in the palaeocurrents at this time. A sudden sea-level rise marked by floodwaters is recorded at the levels from -24.5 to +4.0 m between ca. 8600 and 7800 cal. years BP corresponding to a sea-level rise of around 3.5 m every 100 years. An expiring tide is identified in the early Subboreal affecting the prolific fjord faunas of the Atlantic time.

Original language	English
Pages (from-to)	33-46
Number of pages	14
Journal	Quaternary International
Volume	133-134
DOIs	https://doi.org/10.1016/j.quaint.2004.10.013
Publication status	Published - May 2005

Programme Area

Programme Area 5: Nature and Climate

Access to Document

10.1016/j.quaint.2004.10.013

Cite this

@article{3a442fe5fe4b4c279778322ebcfc0b54,

title = "Main environmental changes since the Weichselian glaciation in the Danish waters between the North Sea and the Baltic Sea as reflected in the molluscan fauna",

abstract = "The Danish waters forming the transition zone between the North Sea and the Baltic Sea are described through changes in the molluscan fauna and bottom communities during the Holocene. The major change in the fauna at the Pleistocene-Holocene boundary is thought to be caused by changes in the palaeocurrents at this time. A sudden sea-level rise marked by floodwaters is recorded at the levels from -24.5 to +4.0 m between ca. 8600 and 7800 cal. years BP corresponding to a sea-level rise of around 3.5 m every 100 years. An expiring tide is identified in the early Subboreal affecting the prolific fjord faunas of the Atlantic time.",

author = "K.S. Petersen and K.L. Rasmussen and Peter Rasmussen and \{von Platen-Hallermund\}, Frants",

note = "Funding Information: Part of this study was supported by a 1-year grant to the senior author from the Carlsberg Foundation. During that year, and subsequently, the Geological Survey of Denmark and Greenland (GEUS) supplied all four authors with research facilities. The support of both these institutions is greatly appreciated. Emily Ryves is thanked for revising the english text. This paper is a contribution to the INQUA Subcommission on Coastal Processes and Sea-level Changes.",

year = "2005",

month = may,

doi = "10.1016/j.quaint.2004.10.013",

language = "English",

volume = "133-134",

pages = "33--46",

journal = "Quaternary International",

issn = "1040-6182",

publisher = "Elsevier",

}

TY - JOUR

T1 - Main environmental changes since the Weichselian glaciation in the Danish waters between the North Sea and the Baltic Sea as reflected in the molluscan fauna

AU - Petersen, K.S.

AU - Rasmussen, K.L.

AU - Rasmussen, Peter

AU - von Platen-Hallermund, Frants

N1 - Funding Information: Part of this study was supported by a 1-year grant to the senior author from the Carlsberg Foundation. During that year, and subsequently, the Geological Survey of Denmark and Greenland (GEUS) supplied all four authors with research facilities. The support of both these institutions is greatly appreciated. Emily Ryves is thanked for revising the english text. This paper is a contribution to the INQUA Subcommission on Coastal Processes and Sea-level Changes.

PY - 2005/5

Y1 - 2005/5

N2 - The Danish waters forming the transition zone between the North Sea and the Baltic Sea are described through changes in the molluscan fauna and bottom communities during the Holocene. The major change in the fauna at the Pleistocene-Holocene boundary is thought to be caused by changes in the palaeocurrents at this time. A sudden sea-level rise marked by floodwaters is recorded at the levels from -24.5 to +4.0 m between ca. 8600 and 7800 cal. years BP corresponding to a sea-level rise of around 3.5 m every 100 years. An expiring tide is identified in the early Subboreal affecting the prolific fjord faunas of the Atlantic time.

AB - The Danish waters forming the transition zone between the North Sea and the Baltic Sea are described through changes in the molluscan fauna and bottom communities during the Holocene. The major change in the fauna at the Pleistocene-Holocene boundary is thought to be caused by changes in the palaeocurrents at this time. A sudden sea-level rise marked by floodwaters is recorded at the levels from -24.5 to +4.0 m between ca. 8600 and 7800 cal. years BP corresponding to a sea-level rise of around 3.5 m every 100 years. An expiring tide is identified in the early Subboreal affecting the prolific fjord faunas of the Atlantic time.

UR - https://www.scopus.com/pages/publications/14244257151

U2 - 10.1016/j.quaint.2004.10.013

DO - 10.1016/j.quaint.2004.10.013

M3 - Article

SN - 1040-6182

VL - 133-134

SP - 33

EP - 46

JO - Quaternary International

JF - Quaternary International

ER -

Main environmental changes since the Weichselian glaciation in the Danish waters between the North Sea and the Baltic Sea as reflected in the molluscan fauna

Abstract

Programme Area

Access to Document

Fingerprint

Cite this