Abstract:
Rare Radiolaria occur in the Upper Cenomanian-Lower Turonian part of finely laminated black shales recovered from Sites 1258 and 1261 of Demerara Rise (Ocean Drilling Program Leg 207, western tropical Atlantic, off Surinam). The observed fauna are of a low diversity, with up to 12 species co-occurring in a single sample and 49 species identified in total in both sites. Nassellarians and "Spumellarians" are equally represented in the assemblages. Diverse species of Stichomitra and Theocampe are particularly common, including the two new species described herein: Theocampe costata and T. demeraraense. Radiolarian preservation is on average moderate to poor, suggesting substantial influence of diagenetic alterations to species diversity. The few well-preserved assemblages can potentially provide better information about Cenomanian-Turonian Radiolarian biodiversity, but given their low abundance in the processed sediment samples, the diversity sampled during this study is considered to be an underestimate of the original Radiolarian diversity at Demerara. However, the abundance and diversity of Theocampe in Upper Cenomanian levels is noteworthy. Given the earliest known occurrence of the genus from Upper Albian sediments of the Deep Ivorian Basin it is likely that it originated and diversified in the opening Equatorial Atlantic Gateway. Based on the stable carbon isotope curve, the OAE-2 interval is clearly identified in the sedimentary sequence of both studied sites and helps to specify the known age range of three species (Acanthocircus hueyi, Archaeospongoprunum bipartitum and Rhopalosyringium hispidum). The most intriguing result of this study is the paucity of Radiolaria within the OAE-2 interval of the deeper site (1258) and the total absence of this micro-zooplankton group in the OAE-2 interval of the proximal site (1261). Radiolaria are the most abundant and diverse at the distal Site 1258, below OAE-2, while the proximal Site 1261 contains very few Radiolaria. The opposite pattern is observed above OAE-2 (few Radiolaria at site 1258, more abundant at site 1261). The paucity or absence of Radiolaria within the OAE-2 interval may be due to the upward excursion of the chemocline in the southern part of the Northern proto-Atlantic. Upwelling of deep warm waters may have fuelled primary productivity (sulfate-reducing bacteria) but prevented at the same time micro-zooplankton survival and proliferation after intensification of euxinic conditions in the surface waters.