Publication Date:
2024-03-07
Description:
Planktonic Foraminifera assemblages register the several climate changes that occurred during the Quaternary. These assemblage variations (frequently abundance reversals) are used to establish bioecozones. Since climate changes are neither synchronic nor spatially homogenous, the purpose is to assess the applicability of the bioecozonations proposed for the Santos and Campos basins in the northern portion of the Pelotas Basin (South Brazilian Continental Margin). The studied grain size was 〉0.150 mm.
Keywords:
Beella digitata; Candeina nitida; Counting, foraminifera, planktic; DEPTH, sediment/rock; Foraminifera, planktic indeterminata; Globigerina bulloides; Globigerina falconensis; Globigerinella calida; Globigerinella siphonifera; Globigerinita glutinata; Globigerinoides conglobatus; Globigerinoides ruber pink; Globigerinoides ruber white; Globigerinoides tenellus; Globoconella inflata; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia menardii; Globorotalia scitula; Globorotalia truncatulinoides dextral; Globorotalia truncatulinoides sinistral; Globorotalia tumida; Globoturborotalita rubescens; Late Quaternary; Neogloboquadrina dutertrei; Neogloboquadrina incompta; Neogloboquadrina pachyderma; Orbulina universa; PC; Piston corer; Planktonic foraminifera; Pulleniatina obliquiloculata; Sample ID; SIS-188; Trilobatus sacculifer; Trilobatus trilobus; Turborotalita quinqueloba; western South Atlantic
Type:
Dataset
Format:
text/tab-separated-values, 690 data points
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