Dinoflagellate cysts in surface sediment samples of METEOR cruises M20/2, M23/1, M34/1, M34/2, M34/3 and M34/4
Citation
Zonneveld K A F, Brune A, Willems H (2000). Dinoflagellate cysts in surface sediment samples of METEOR cruises M20/2, M23/1, M34/1, M34/2, M34/3 and M34/4. PANGAEA - Publishing Network for Geoscientific and Environmental Data. Occurrence dataset https://doi.org/10.1594/pangaea.85167 accessed via GBIF.org on 2022-12-04.Description
To enhance the limited information available about the palaeo-ecological significance of calcareous dinoflagellates, we have studied their lateral distribution in surface sediments of the equatorial and south Atlantic between 13°N and 36°S. Calcareous dinoflagellate cysts appear to be widely distributed throughout the studied area. In the surface sediments, concentrations (cyst per gram dry sediment) of the vegetative stage Thoracosphaera heimii are generally higher than that of the (presumably) calcareous resting cysts. Distribution patterns in surface sediments of Orthopithonella granifera (Fütterer) Keupp and Versteegh, Rhabdothorax spp. Kamptner., Sphaerodinella albatrosiana (Kamptner) Keupp and Versteegh S. albatrosiana praratabulated, Sphaerodinella tuberosa var. 1 (Kamptner) Keupp and Versteegh and S. tuberosa var. 2 and the ratios between these species have been compared with temperature, salinity, density and stratification gradients in the upper water column. Rhabdothorax spp. is characteristically present in sediments of more temperate regions characterized by high seasonality. Dinoflagellates producing these cysts are able to tolerate high nutrient concentrations, and mixing of the water column. S. albatrosiana is abundant in regions characterized by high sea surface temperatures and oligotrophic surface water conditions. In contrast, the distribution of S. tuberosa var. 2 is negatively related to temperature. The other cyst species did not show a characteristic pattern in relation to the studied environmental gradients. The ratio of Sphaerodinella tuberosa var. 2 to Orthopithonella granifera can be used for reconstructing the presence of stratification in the upper 50 m of the water column, whereas the ratios of S. tuberosa var. 2 to Sphaerodinella albatrosiana and of O. granifera to Rhabdothorax spp. might be used for palaeotemperature reconstructions. Calcareous dinoflagellate cysts are abundant in oligotrophic areas and may be useful for the reconstruction of palaeoenvironmental conditions.Taxonomic Coverages
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Chromistarank: kingdom
Geographic Coverages
Event: GeoB1703-3,
off Kunene
; Event: GeoB1704-2,
Walvis Ridge
; Event: GeoB1705-2,
Walvis Ridge
; Event: GeoB1706-1,
Walvis Ridge
; Event: GeoB1707-2,
Walvis Ridge
; Event: GeoB1710-1,
Namibia continental slope
; Event: GeoB1711-6,
Namibia continental slope
; Event: GeoB1712-1,
Namibia continental slope
; Event: GeoB1713-5,
Namibia continental slope
; Event: GeoB1714-1,
Namibia Continental Margin
; Event: GeoB1715-1,
Namibia Continental Margin
; Event: GeoB1716-2,
Namibia Continental Margin
; Event: GeoB1717-2,
Namibia Continental Margin
; Event: GeoB1718-1,
Namibia Continental Margin
; Event: GeoB1719-4,
Namibia continental slope
; Event: GeoB1720-4,
Namibia Continental Margin
; Event: GeoB1721-4,
Namibia Continental Margin
; Event: GeoB1722-3,
Namibia Continental Margin
; Event: GeoB1724-3,
Namibia continental slope
; Event: GeoB1728-3,
Namibia Continental Margin
; Event: GeoB1729-1,
Namibia Continental Margin
; Event: GeoB2001-1,
South African margin
; Event: GeoB2007-1,
Cape Basin
; Event: GeoB2008-1,
Cape Basin
; Event: GeoB2009-1,
Cape Basin
; Event: GeoB2011-1,
Cape Basin
; Event: GeoB3601-1,
Southern Cape Basin
; Event: GeoB3602-2,
Southern Cape Basin
; Event: GeoB3603-1,
Southern Cape Basin
; Event: GeoB3604-4,
Southern Cape Basin
; Event: GeoB3605-1,
Southern Cape Basin
; Event: GeoB3606-2,
Northern Cape Basin
; Event: GeoB3607-1,
Northern Cape Basin
; Event: GeoB3608-1,
Northern Cape Basin
; Event: GeoB3715-1,
Northern Cape Basin
; Event: GeoB3717-1,
Northern Cape Basin
; Event: GeoB3718-8,
Northern Cape Basin
; Event: GeoB3719-2,
Northern Cape Basin
; Event: GeoB3720-3,
Northern Cape Basin
; Event: GeoB3721-4,
Northern Cape Basin
; Event: GeoB3723-2,
Northern Cape Basin
; Event: GeoB3724-1,
Northern Cape Basin
; Event: GeoB3801-5,
Mid Atlantic Ridge
; Event: GeoB3802-2,
Mid Atlantic Ridge
; Event: GeoB3803-1,
Mid Atlantic Ridge
; Event: GeoB3804-2,
Mid Atlantic Ridge
; Event: GeoB3806-2,
Mid Atlantic Ridge
; Event: GeoB3807-2,
Mid Atlantic Ridge
; Event: GeoB3808-7,
Mid Atlantic Ridge
; Event: GeoB3809-1,
Mid Atlantic Ridge
; Event: GeoB3810-2,
Mid Atlantic Ridge
; Event: GeoB3812-2,
Mid Atlantic Ridge
; Event: GeoB3822-1,
Vema Channel
; Event: GeoB3825-1,
Continental slope off Brazil
; Event: GeoB3826-2,
Continental slope off Brazil
; Event: GeoB3827-1,
Continental slope off Brazil
; Event: GeoB3906-9,
Brazil Basin
; Event: GeoB3908-11,
Equatorial Atlantic
; Event: GeoB3909-1,
Northeast Brasilian Margin
; Event: GeoB3910-3,
Northeast Brasilian Margin
; Event: GeoB3911-1,
Northeast Brasilian Margin
; Event: GeoB3912-2,
Northeast Brasilian Margin
; Event: GeoB3913-2,
Northeast Brasilian Margin
; Event: GeoB3914-3,
Northeast Brasilian Margin
; Event: GeoB3916-1,
Amazon Shelf/Fan
; Event: GeoB3918-1,
Amazon Shelf/Fan
; Event: GeoB3925-2,
Amazon Shelf/Fan
; Event: GeoB3935-1,
Atlantic Caribbean Margin
; Event: GeoB3936-2,
Atlantic Caribbean Margin
; Event: GeoB3937-1,
Atlantic Caribbean Margin
; Event: GeoB3938-2,
Atlantic Caribbean Margin
; Event: GeoB3939-1,
Atlantic Caribbean Margin
;
Bibliographic Citations
Contacts
Karin A F Zonneveldoriginator
Anja Brune
originator
Helmut Willems
originator
metadata author
PANGAEA - Data Publisher for Earth & Environmental Science
email: info@pangaea.de
homepage: https://www.pangaea.de
administrative point of contact
PANGAEA - Data Publisher for Earth & Environmental Science
email: info@pangaea.de
homepage: http://www.pangaea.de