Planktonic foraminifera census counts from the western South Atlantic, supplement to: García Chapori, Natalia Luz; Laprida, Cecilia (2021): Planktonic foraminifera assemblages from the Brazil–Malvinas Confluence: palaeoceanographic implications of sub‐surface temperature reconstructions in the western South Atlantic. Lethaia

• Main Authors: García Chapori, Natalia Luz, Kucera, Michal
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
• Subjects: Event label; Latitude of event; Longitude of event; Elevation of event; Ocean; DEPTH, sediment/rock; Depth, top/min; Depth, bottom/max; Orbulina universa; Globigerinoides conglobatus; Globigerinoides ruber pink; Globigerinoides ruber white; Globigerinoides tenellus; Trilobatus sacculifer; Globigerinella siphonifera; Globigerinella calida; Globigerina bulloides; Globigerina falconensis; Beella digitata; Globoturborotalita rubescens; Turborotalita quinqueloba; Neogloboquadrina pachyderma; Neogloboquadrina incompta; Neogloboquadrina dutertrei; Pulleniatina obliquiloculata; Globoconella inflata; Globorotalia truncatulinoides; Globorotalia hirsuta; Globorotalia scitula; Globorotalia menardii; Globorotalia tumida; Candeina nitida; Globigerinita glutinata; Globigerinita uvula; Foraminifera, planktic indeterminata; Foraminifera, planktic; Giant box corer; MultiCorer; Gravity corer Kiel type; Counting >150 µm fraction; M29/1; M46/2; M46/3; Meteor 1986; Center for Marine Environmental Sciences MARUM; Laprida; Planktonic foraminifera
• Online Access: https://dx.doi.org/10.1594/pangaea.907931; https://doi.pangaea.de/10.1594/PANGAEA.907931

Planktonic foraminifera census data have been widely used to reconstruct changes in ocean ecosystems as well as ocean chemistry and circulation through calibration functions. Here we analyse new core‐top census data from 22 sites in the western South Atlantic, improving the geographical coverage and spatial resolution of the environmental gradients from the region covered by the Brazil–Malvinas Confluence (~38°S–53°W). We combine them with previous data to provide an up‐to‐date compilation of the western South Atlantic planktonic foraminifera–calibration data set. We study the relationship between the assemblages present in the core‐top samples and the most dynamic environmental variables from the region to establish the environmental variable(s) more resolved by the assemblages. Therefore, we develop and assess a new calibration function using the data set and testing several statistical models at different water depths. Our results reveal that the distribution and abundance of the species in the Brazil–Malvinas Confluence region mainly reflect the influence of two environmental variables: the mixed layer temperature and mixed layer depth (57% of total variance). The most precise reconstructions were obtained when using sub‐surface temperatures between 40 and 50 m water depth. The application of the calibration function to a Holocene sediment core at ~37°S–53°W revealed mean annual sub‐surface temperature reconstructions between 8°C and 11°C, confirming the northward displacement of the Brazil–Malvinas Confluence during the onset of the Holocene and suggesting a major influence of the Malvinas Current during the entire Holocene at the studied site.