

FOLLOWUS
1. School of Life Sciences Xiamen University
2. Hainan Provincial Marine Development Plan and Design Research Institute
3. State Key Laboratory of Marine Environmental Science Xiamen University
4. Third Institute of Oceanography SOA
网络首发:2013-01-16,
纸质出版:2013
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Diatom assemblages in surface sediments from the South China Sea as environmental indicators[J]. 海洋湖沼学报(英文), 2013,31(1):31-45.
Wu, R., Gao, Y., Fang, Q. et al. Diatom assemblages in surface sediments from the South China Sea as environmental indicators., Chin. J. Ocean. Limnol. 31, 31–45 (2013). https://doi.org/10.1007/s00343-013-1181-8
Diatom assemblages in surface sediments from the South China Sea as environmental indicators[J]. 海洋湖沼学报(英文), 2013,31(1):31-45. DOI: 10.1007/s00343-013-1181-8.
Wu, R., Gao, Y., Fang, Q. et al. Diatom assemblages in surface sediments from the South China Sea as environmental indicators., Chin. J. Ocean. Limnol. 31, 31–45 (2013). https://doi.org/10.1007/s00343-013-1181-8 DOI:
We studied diatom distribution from 62 samples from the uppermost 1 cm of sediment in the South China Sea (SCS)
using grabs or box corers in three cruises between 2001–2007. Fifty six genera
256 species and their varieties were identified. Dominating species included Coscinodiscus africanus
Coscinodiscus nodulifer
Cyclotella stylorum
Hemidiscus cuneiformis
Melosira sulcata
Nitzschia marina
Roperia tesselata
Thalassionema nitzschioides
Thalassiosira excentrica
and Thalassiothrix longissima. Most surface sediments in the SCS were rich in diatoms
except for a few coarse samples. Average diatom abundance in the study area was 104 607 valve/g. In terms of the abundance
ecology
and spatial distribution
seven diatom zones (Zones 1–7) were recognized. Zone 1 (northern continental shelf) is affected by warm currents
SCS northern branch of the Kuroshio
and northern coastal currents; Zone 2 (northwestern continental shelf) is affected by intense coastal currents; Zone 3 (Xisha Islands sea area) is a bathyal environment with transitional water masses; Zone 4 (sea basin) is a bathyal-to-deep sea with stable and uniform central water masses in a semi-enclosed marginal sea; Zone 5 (Nansha Islands marine area) is a pelagic environment with relatively high surface temperature; Zone 6 (northern Sunda Shelf) is a tropical shelf environment; and Zone 7 (northern Kalimantan Island shelf area) is affected by warm waters from the Indian Ocean and coastal waters. The data indicate that these diatom zones are closely related to topography
hydrodynamics
temperature
nutrients and especially the salinity. Better understanding of the relationship between diatom distribution and the oceanographic factors would help in the reconstruction of the SCS in the past.
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