MENARDIIFORM PLANKTONIC FORAMINIFERA STRATIGRAPHY FROM MIDDLE PLEISTOCENE TO HOLOCENE IN THE WESTERN SOUTH ATLANTIC

Autor(es)

Costa, Karen Badaraco ^[1] ; Camillo Jr, Edmundo ; Aoki Santarosa, Ana Claudia ^[2] ; Iwai, Fabiane Sayuri ^[2] ; de Quadros, Juliana Pereira ^[3] ; Leipnitz, Itamar Ivo ^[4] ; de Lima Toledo, Felipe Antonio ^[2]

Afiliação do(s) autor(es)

^[1] Univ Sao Paulo, Lab Paleoceanog Atlantico Sul, Inst Oceanog, LaPAS, Praca Oceanog 191, Cidade Univ, BR-05580120 Sao Paulo, SP - Brazil

^[2] Camillo Jr, Jr., Edmundo, Univ Sao Paulo, Lab Paleoceanog Atlantico Sul, Inst Oceanog, LaPAS, Praca Oceanog 191, Cidade Univ, BR-05580120 Sao Paulo, SP - Brazil

^[3] Univ Fed Sul Bahia, Inst Humanidades Artes & Ciencias, Ctr Formacao Ciencias Ambientais, CFCAm, Rodovia BR-367 Km 10 S-N, BR-45810000 Porto Seguro, BA - Brazil

^[4] Univ Vale Rio dos Sinos, Inst Tecnol Micropaleontol, ITT FOSSIL UNISINOS, Av Unisinos 950, BR-93022000 Sao Leopoldo, RS - Brazil

• Tipo de documento: Artigo Científico
• Fonte: Revista Brasileira de Paleontologia; v. 21, n. 3, p. 225-237, SEP-DEC 2018.
• Citações Web of Science: 1

Resumo

We studied the Middle Pleistocene to Holocene menardiiform planktonic foraminifera (MPF) stratigraphy in six continuous deep-sea sediment cores recovered from the Brazilian continental slope to evaluate its use in climatic characterization and as a reliable biostratigraphic tool in the western South Atlantic. For this purpose, an important issue was to construct a robust local biochronological framework for the past 772 ky in the western South Atlantic (Santos Basin). The oxygen isotope chronostratigraphic control allowed us to recalibrate the MPF events in the Santos Basin and identify diachronous bioevents. The bio-horizons found in the Santos Basin, such as the V/W and T/U (bio)zone boundaries, were found in a different chronostratigraphic position compared to previous studies. Results indicate that typical cyclic disappearances and reappearances of the MPF are not synchronous throughout the Atlantic Ocean and should not be employed for `climatic zonation'. This asynchronous evidence also provides information on the timing of the mechanisms responsible for the proliferation of these species throughout the Atlantic Ocean. Therefore, we strongly recommend that a local biochronological framework should be used for inter-basin comparisons and also accumulation rate estimates, both for paleoclimatic studies and continental slope geohazard assessment. (AU)

• Processo FAPESP: 13/50224-2 - High resolution climate record for the last climatic cycle in the subtropical SW Atlantic
• Beneficiário: Karen Badaraco Costa
• Modalidade de apoio: Auxílio à Pesquisa - Regular