_version_ 1867170879263211520
author Widmark, Joen G V
Malmgren, Bjorn
author_facet Widmark, Joen G V
Malmgren, Bjorn
collection Datos científicos de ciencias marinas y ambientales
contents Material from the Deep Sea Drilling Project (DSDP) Site 527 from the Angola Basin, South Atlantic Ocean, has been analyzed to determine whether Upper Cretaceous benthonic foraminiferal taxa are differentially sensitive to calcite dissolution, and, if so, to rank their order of susceptibility. Two regimes of dissolution, established on the basis of the degree of planktonic foraminiferal fragmentation, representing stronger and less prominent dissolution within the section studied, were used as a framework for reference. A total of 60 calcareous and eight agglutinated benthonic foraminiferal taxa were identified at the species or genus level; of these, twenty-three calcareous and five agglutinated taxa were selected for the dissolution study. Relative abundance of each of the various taxa was tested statistically, using t-test, between dissolution regimes to assess the significance of the change induced by increased dissolution. Nuttallides truempyi and Neoeponides sp. intermediate form are interpreted as resistant to dissolution. Pullenia spp., Alabamina sp. a, Anomalina sp. a, Praebulimina sp. fusiform, and Nuttallinella sp. a are susceptible to dissolution. The majority of the taxa (16 in number) are unaffected by dissolution because they show no change between dissolution regimes. Among the agglutinated taxa Gaudryina pyramidata is resistant to dissolution, whereas the remaining four taxa are unaffected by dissolution. At the level of superfamilies, one calcareous superfamily (Discorbacea) is resistant, two (Orbitoidacea and Cassidulinacea) are unaffected, and two (Nodosariacea and Buliminacea) are susceptible to dissolution.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_687437
institution PANGAEA
language en
publishDate 1988
publisher PANGAEA
record_format pangaea
spellingShingle Benthic foraminiferal assemblages of Upper Cretaceous sediments from DSDP Hole 74-527 in the Angola Basin, South Atlantic Ocean (Table I, Appendix II)
Widmark, Joen G V
Malmgren, Bjorn
74-527; Alabamina sp.; Anomalina praeacuta; Anomalina sp.; Buliminacea; Buliminella beaumonti; Cassidulinacea; Cibicidoides spp.; Counting >125 µm fraction; Deep Sea Drilling Project; Dentalina spp.; DEPTH, sediment/rock; Discorbacea; Dorothia trochoides; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Foraminifera, benthic, fragments; Foraminifera, benthic agglutinated; Foraminifera, benthic indeterminata; Gaudryina pyramidata; Gavelinella beccariiformis; Gavelinella hyphalus; Globulina lacrima; Glomar Challenger; Gyroidinoides quadratus; Gyroidinoides spp.; Leg74; Neoeponides hillebrandti; Neoeponides lunata; Neoeponides sp.; Nodosariaceae; Nuttallides sp.; Nuttallides truempyi; Nuttallinella sp.; Orbitoidacea; Oridorsalis umbonatus; Osangularia spp.; Praebulimina sp.; Pullenia spp.; Reussella szajnochae; Sample code/label; Sample code/label 2; Sample mass; South Atlantic Ocean; Spiroplectammina dentata; Spiroplectammina spp.; Tritaxia spp.
Material from the Deep Sea Drilling Project (DSDP) Site 527 from the Angola Basin, South Atlantic Ocean, has been analyzed to determine whether Upper Cretaceous benthonic foraminiferal taxa are differentially sensitive to calcite dissolution, and, if so, to rank their order of susceptibility. Two regimes of dissolution, established on the basis of the degree of planktonic foraminiferal fragmentation, representing stronger and less prominent dissolution within the section studied, were used as a framework for reference. A total of 60 calcareous and eight agglutinated benthonic foraminiferal taxa were identified at the species or genus level; of these, twenty-three calcareous and five agglutinated taxa were selected for the dissolution study. Relative abundance of each of the various taxa was tested statistically, using t-test, between dissolution regimes to assess the significance of the change induced by increased dissolution. Nuttallides truempyi and Neoeponides sp. intermediate form are interpreted as resistant to dissolution. Pullenia spp., Alabamina sp. a, Anomalina sp. a, Praebulimina sp. fusiform, and Nuttallinella sp. a are susceptible to dissolution. The majority of the taxa (16 in number) are unaffected by dissolution because they show no change between dissolution regimes. Among the agglutinated taxa Gaudryina pyramidata is resistant to dissolution, whereas the remaining four taxa are unaffected by dissolution. At the level of superfamilies, one calcareous superfamily (Discorbacea) is resistant, two (Orbitoidacea and Cassidulinacea) are unaffected, and two (Nodosariacea and Buliminacea) are susceptible to dissolution.
title Benthic foraminiferal assemblages of Upper Cretaceous sediments from DSDP Hole 74-527 in the Angola Basin, South Atlantic Ocean (Table I, Appendix II)
topic 74-527; Alabamina sp.; Anomalina praeacuta; Anomalina sp.; Buliminacea; Buliminella beaumonti; Cassidulinacea; Cibicidoides spp.; Counting >125 µm fraction; Deep Sea Drilling Project; Dentalina spp.; DEPTH, sediment/rock; Discorbacea; Dorothia trochoides; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Foraminifera, benthic, fragments; Foraminifera, benthic agglutinated; Foraminifera, benthic indeterminata; Gaudryina pyramidata; Gavelinella beccariiformis; Gavelinella hyphalus; Globulina lacrima; Glomar Challenger; Gyroidinoides quadratus; Gyroidinoides spp.; Leg74; Neoeponides hillebrandti; Neoeponides lunata; Neoeponides sp.; Nodosariaceae; Nuttallides sp.; Nuttallides truempyi; Nuttallinella sp.; Orbitoidacea; Oridorsalis umbonatus; Osangularia spp.; Praebulimina sp.; Pullenia spp.; Reussella szajnochae; Sample code/label; Sample code/label 2; Sample mass; South Atlantic Ocean; Spiroplectammina dentata; Spiroplectammina spp.; Tritaxia spp.
url https://doi.org/10.1594/PANGAEA.687437