Coccolith distribution patterns in South Atlantic and Southern Ocean surface sediments in relation to environmental gradients

被引:86
作者
Boeckel, Babette
Baumann, Karl-Heinz
Henrich, Ruediger
Kinkel, Hanno
机构
[1] Univ Bremen, Fac 05, D-28334 Bremen, Germany
[2] Univ Kiel, Inst Geosci, D-24098 Kiel, Germany
关键词
coccoliths; distribution; ecology; statistics; surface sediments; South Atlantic; Southern Ocean (Atlantic sector);
D O I
10.1016/j.dsr.2005.11.006
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
In this study, the coccolith compositions of 213 surface sediment samples from the South Atlantic and Southern Ocean were analysed with respect to the environmental parameters of the overlying surface waters. From this data set, the abundance patterns of the main species and their ecological affinities were ascertained. In general, Emiliania huxleyi is the most abundant species of the recent coccolith assemblages in the study region. However, the lower photic zone taxa, composed of Florisphaera profunda and Gladiolithus flabellatus often dominate the assemblages between 20 degrees N and 30 degrees S. If E huxleyi is excluded, Calcidiscus leptoporus and F. profunda become the most abundant species, each dominating discrete oceanographic regimes. While F. profunda is very abundant in the sediments underneath warmer, stratified surface waters with a deep nutricline, Calcidiscus leptoporus is encountered in high-productivity environments. Furthermore, the results of a canonical correspondence analysis reveal affinities of Gephyrocapsa spp., Helicosphaera spp. and Coccolithus pelagicus for intermediate to higher nutrient conditions in a well-mixed upper water column. In contrast, Gladiolithus flabellatus seems to be associated with high temperatures and salinities under low-nutrient conditions. Based on the relative abundances of Calcidiscus leptoporus, F. profunda, Gladiolithus flabellatus, Helicosphaera spp., Umbilicosphaera foliosa, Umbilicosphaera sibogae and a group of subordinate subtropical species, six surface sediment assemblages have been identified, which reflect the distribution and characteristics of the overlying surface waters. Their distribution appears to be mainly a function of the relative position of the nutricline and thermocline in the overlying photic zone. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1073 / 1099
页数:27
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