Planktonic foraminiferal diversity, equitability and biostratigraphic analysis of samples from Ocean Drilling Program (ODP) Leg 122, Hole 762C show that in general, cool water conditions prevailed during the latest Campanian–Maastrichtian in the eastern Indian Ocean. This is indicated by planktonic foraminiferal assemblages characterized by low species diversity and equitability with abundant rugoglobigerinids and heterohelicids. Archaeoglobigerinids, globigerinelloids, hedbergellids, and long-ranging double-keeled globotruncanids are also present in varying abundance but single-keeled forms occur rarely and sporadically. Identification of the stage and zonal boundaries for the studied geologic interval have been achieved through biostratig...
The biogeographic distribution of planktonic foraminifera from southern mid-to high latitudes region...
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Ind...
Neogene calcareous sediments were recovered at 12 sites in the western Indian Ocean (Table 1). Appro...
The distribution of 79 foraminiferal species is recorded among 23 samples taken from Cores 123-776A-...
A biostratigraphically complete upper Maestrichtian-Danian sequence was recovered at ODP Leg 119 Sit...
Hole 997A was drilled during Leg 164 of the Ocean Drilling Program at a depth of 2770 m on the topog...
Late Campanian and Maastrichtian benthic foraminifers are recorded from 12 samples from Ocean Drilli...
Deep-sea benthic foraminifera have been quantitatively analyzed in samples (>125 µm size fraction) f...
We present a high-resolution (6 k.y. sample interval) record of planktonic foraminifer faunal variat...
The evolution of planktonic foraminifera during the Late Cretaceous is marked in the Santonian by th...
Planktonic foraminifera from Pliocene - Early Quaternary sediments of ODP Hole 111-677A were studied...
Late Neogene planktonic foraminiferal biostratigraphy of DSDP Site 296, Leg 31, reveals this site as...
The evolution of planktonic foraminifera during the Late Cretaceous is marked in the Santonian by th...
Planktonic foraminifers from DSDP Site 586 on Leg 89 and Sites 587-594 on Leg 90, cored by the Gloma...
Tropical climate is variable on astronomical time scale, driving changes in surface and deep-sea fau...
The biogeographic distribution of planktonic foraminifera from southern mid-to high latitudes region...
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Ind...
Neogene calcareous sediments were recovered at 12 sites in the western Indian Ocean (Table 1). Appro...
The distribution of 79 foraminiferal species is recorded among 23 samples taken from Cores 123-776A-...
A biostratigraphically complete upper Maestrichtian-Danian sequence was recovered at ODP Leg 119 Sit...
Hole 997A was drilled during Leg 164 of the Ocean Drilling Program at a depth of 2770 m on the topog...
Late Campanian and Maastrichtian benthic foraminifers are recorded from 12 samples from Ocean Drilli...
Deep-sea benthic foraminifera have been quantitatively analyzed in samples (>125 µm size fraction) f...
We present a high-resolution (6 k.y. sample interval) record of planktonic foraminifer faunal variat...
The evolution of planktonic foraminifera during the Late Cretaceous is marked in the Santonian by th...
Planktonic foraminifera from Pliocene - Early Quaternary sediments of ODP Hole 111-677A were studied...
Late Neogene planktonic foraminiferal biostratigraphy of DSDP Site 296, Leg 31, reveals this site as...
The evolution of planktonic foraminifera during the Late Cretaceous is marked in the Santonian by th...
Planktonic foraminifers from DSDP Site 586 on Leg 89 and Sites 587-594 on Leg 90, cored by the Gloma...
Tropical climate is variable on astronomical time scale, driving changes in surface and deep-sea fau...
The biogeographic distribution of planktonic foraminifera from southern mid-to high latitudes region...
Middle Miocene (14.8–11.9 Ma) deep-sea sediments from ODP Hole 747A (Kerguelen Plateau, southern Ind...
Neogene calcareous sediments were recovered at 12 sites in the western Indian Ocean (Table 1). Appro...