Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Geological Magazine   Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geological Magazine; January 2006; v. 143; no. 1; p. 105-114; DOI: 10.1017/S0016756805001408
© 2006 Cambridge University Press (CUP)
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by LÖWEMARK, L.
Right arrow Articles by SARNTHEIN, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Temporal variations of the trace fossil Zoophycos in a 425 ka long sediment record from the South China Sea: implications for the ethology of the Zoophycos producer

LUDVIG LÖWEMARK*,*, HUI-LING LIN{dagger} and MICHAEL SARNTHEIN{ddagger}

* Department of Geosciences, National Taiwan University, P.O. Box 13-318, Taiwan ROC
{dagger} Institute of Marine Geology and Chemistry, National Sun Yat-Sen University, Kaoshiung 804, Taiwan ROC
{ddagger} Institut für Geowissenschaften, Universiät at Kiel, Olshausenstr. 40, D-24118 Kiel, Germany

* Corresponding author: ludvig{at}ntu.edu.tw; previously at Institute of Earth Sciences, Academia Sinica, P.O. Box 1-55, Nankang, Taipei 115, Taiwan ROC.

A 425 ka long record from piston core GIK17925-3 taken in the northeastern South China Sea was used to study the environmental conditions controlling the distribution of the Zoophycos trace fossil. The 12 m long core offers a unique opportunity to study the response of the Zoophycos-producing animal to environmental variations over four glacial–interglacial cycles. The trace fossils show a strong glacial to interglacial variation in their abundance with a special preference for intervals with low sedimentation rates. Additional X-ray radiograph studies of piston cores from the Southeast Asian Marginal Seas show that the trace fossil Zoophycos is widespread in slope and deep-marine sediments, with the highest abundances encountered in low sedimentation rate settings. The preference of the Zoophycos producer for low sedimentation rates in a setting with strong seasonal fluctuations in food supply due to the shift between winter and summer monsoons, is interpreted to be the result of a cache-model behaviour, where food is collected during rich times and squirrelled away for poor times. Core GIK17925-3 also offers an opportunity to assess the impact of Zoophycos bioturbation on various palaeoenvironmental proxies. In this core, more than 30 % of the measured data points were more or less strongly affected by Zoophycos bioturbation. Together with the widespread occurrence this percentage indicates that Zoophycos may pose a serious threat to palaeoclimatic reconstructions in cores from low to moderate sedimentation rate sites.

Key Words: Zoophycos • South China Sea • Quaternary • ichnofossils • lebensspuren




This article has been cited by other articles:


Home page
Geological MagazineHome page
Y.-M. GONG, G. R. SHI, E. A. WELDON, Y.-S. DU, and R. XU
Pyrite framboids interpreted as microbial colonies within the Permian Zoophycos spreiten from southeastern Australia
Geological Magazine, January 1, 2008; 145(1): 95 - 103.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Cambridge University Press (CUP)