(Figure 4) Stratigraphic distribution of planktonic foraminifera in DSDP Hole 93-604 ...

• Main Author: Moullade, Michel
• Format: Dataset
• Language: English
• Published: PANGAEA 1987
• Subjects: Epoch; Planktic foraminifera zone; Sample code/label; DEPTH, sediment/rock; Globorotalia tumida; Globorotalia menardii; Globorotalia inflata; Globorotalia crassaformis; Globorotalia truncatulinoides; Pulleniatina finalis; Pulleniatina obliquiloculata; Neogloboquadrina dutertrei; Globigerinoides ruber var. alba; Globigerinoides ruber roseus; Neogloboquadrina pachyderma; Globigerinoides quadrilobatus trilobatus; Globigerinoides conglobatus; Globigerina bulloides; Orbulina universa; Globigerinita glutinata; Globorotalia hirsuta; Globigerinoides obliquus; Globigerinoides quadrilobatus sacculifer; Globorotalia scitula; Sphaeroidinella dehiscens; Globorotalia tosaensis; Neogloboquadrina humerosa; Globorotalia ungulata; Neogloboquadrina acostaensis; Globorotalia miocenica; Neogloboquadrina cf. atlantica; Globorotalia praemiocenica; Globorotalia praehirsuta; Globorotalia puncticulata; Sphaeroidinellopsis seminulina; Globoquadrina altispira; Globorotalia margaritae; Globigerina nepenthes; Sphaeroidinellopsis paenedehiscens; Globorotalia plesiotumida; Globorotalia merotumida; Orbulina suturalis; Globigerina praebulloides; Drilling/drill rig; DSDP/ODP/IODP sample designation; Leg93; Glomar Challenger; Deep Sea Drilling Project DSDP; North Atlantic; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.250663; https://doi.pangaea.de/10.1594/PANGAEA.250663

During Deep Sea Drilling Project Leg 93, upper Miocene through Quaternary sediments were continuously cored in Hole 604, located on the upper continental rise of the New Jersey transect (western North Atlantic). A detailed biostratigraphic study of these strata has been made using the vertical distribution of planktonic foraminifers. The Quaternary climatic zonation of Ericson and Wollin (1968) has been tentatively delineated and all the Pliocene zones and subzones (sensu Berggren, 1977) have been recognized. The rate of sedimentation was slow during most of the Pliocene but underwent a significant acceleration in the early Pleistocene. Quantitative variations in the distribution of planktonic foraminifers appear to be influenced by various factors, such as hydrodynamic winnowing resulting from the action of bottom currents and surficial thermal conditions caused by climatic changes. Both dissolution intervals and brief increases in the coarser detrital input seem, most of the time, to be correlated with ... : Species abundance: A = abundant, C = common, F = few, R = rare, VR = very rare, - = absent. ...