TY - JOUR
T1 - Distribution of dinocyst assemblages in surface sediment samples from the West Greenland margin
AU - Allan, Estelle
AU - de Vernal, Anne
AU - Krawczyk, Diana
AU - Moros, Matthias
AU - Radi, Taoufik
AU - Rochon, André
AU - Seidenkrantz, Marit Solveig
AU - Zaragosi, Sébastien
PY - 2020/8
Y1 - 2020/8
N2 - ( )Palynological analyses of 60 surface sediment samples from West Greenland margin revealed high concentrations of dinoflagellate cysts (dinocysts), particularly in the Disko Bugt area, where they reach > 10(4) cysts g(-1). Dinocyst assemblages are characterized by a relatively high species diversity and are dominated by Operculodinium centrocarpum, cysts of Pentapharsodinium dalei, Islandinium minutum, Islandinium? cezare, and Brigantedinium spp. On a regional scale, the overall assemblages show statistical relationships with sea-ice cover duration, primary productivity, salinity and summer-fall temperature. The cysts of Pentapharsodinium dalei, Operculodinium centrocarpum, and Spiniferites elongatus appear linked to high productivity and to characterize the late summer-fall bloom. Although Islandinium minutum and Islandinium? cezare are generally associated with a seasonally sea-ice covered environment, there is no linear relationship between their relative abundance and seaice concentration or duration on a regional scale, along the West Greenland margin. The abundance of these taxa primarily reflects cold and low-salinity water in the study area. Radionuclide measurements (Pb-210 and Cs-137) allow the distinction between two categories of samples, the "modern" ones likely encompassing the interval younger than 1950 CE, and the others that may be considered "sub-modern". Statistical analyses indicate that dinocyst assemblages belonging to "modern" and "sub-modern" categories are not significantly different. Hence, the dinocyst assemblages of surface sediment samples, both "modern" and "sub-modern", represent fluxes homogenized over a relatively long time interval, which illustrates a spatial distribution corresponding to the main gradient in oceanographic conditions. Consequently, dinocyst assemblages in surface sediments can be assumed to represent the average "modern" conditions with a sufficiently high degree of confidence for their use in environmental studies and paleoclimate reconstructions.
AB - ( )Palynological analyses of 60 surface sediment samples from West Greenland margin revealed high concentrations of dinoflagellate cysts (dinocysts), particularly in the Disko Bugt area, where they reach > 10(4) cysts g(-1). Dinocyst assemblages are characterized by a relatively high species diversity and are dominated by Operculodinium centrocarpum, cysts of Pentapharsodinium dalei, Islandinium minutum, Islandinium? cezare, and Brigantedinium spp. On a regional scale, the overall assemblages show statistical relationships with sea-ice cover duration, primary productivity, salinity and summer-fall temperature. The cysts of Pentapharsodinium dalei, Operculodinium centrocarpum, and Spiniferites elongatus appear linked to high productivity and to characterize the late summer-fall bloom. Although Islandinium minutum and Islandinium? cezare are generally associated with a seasonally sea-ice covered environment, there is no linear relationship between their relative abundance and seaice concentration or duration on a regional scale, along the West Greenland margin. The abundance of these taxa primarily reflects cold and low-salinity water in the study area. Radionuclide measurements (Pb-210 and Cs-137) allow the distinction between two categories of samples, the "modern" ones likely encompassing the interval younger than 1950 CE, and the others that may be considered "sub-modern". Statistical analyses indicate that dinocyst assemblages belonging to "modern" and "sub-modern" categories are not significantly different. Hence, the dinocyst assemblages of surface sediment samples, both "modern" and "sub-modern", represent fluxes homogenized over a relatively long time interval, which illustrates a spatial distribution corresponding to the main gradient in oceanographic conditions. Consequently, dinocyst assemblages in surface sediments can be assumed to represent the average "modern" conditions with a sufficiently high degree of confidence for their use in environmental studies and paleoclimate reconstructions.
KW - Dinocysts
KW - Primary production
KW - Sea-surface conditions
KW - West Greenland
UR - http://www.scopus.com/inward/record.url?scp=85077709124&partnerID=8YFLogxK
U2 - 10.1016/j.marmicro.2019.101818
DO - 10.1016/j.marmicro.2019.101818
M3 - Journal article
AN - SCOPUS:85077709124
SN - 0377-8398
VL - 159
JO - Marine Micropaleontology
JF - Marine Micropaleontology
M1 - 101818
ER -