Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz
For planktonic foraminifera counts, 9–12 cc of 68 bulk sub-samples were wet-weighed, freeze-dried, and re-weighed, then ultra-sonicated in a water bath, washed and sieved with tap and distilled water at the end through two grain-size fractions (63–150 μm and >150 μm) at the IGME. These fractions...
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2024
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.966840 2024-09-15T18:19:24+00:00 Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel LATITUDE: 34.971330 * LONGITUDE: -6.841170 * MINIMUM DEPTH, sediment/rock: 0.010 m * MAXIMUM DEPTH, sediment/rock: 2.125 m 2024 text/tab-separated-values, 162 data points https://doi.pangaea.de/10.1594/PANGAEA.966840 https://doi.org/10.1594/PANGAEA.966840 en eng PANGAEA https://doi.org/10.1594/PANGAEA.966606 Lebreiro, Susana Martin; Antón López, Laura; Reguera, Maria Isabel; Marzocchi, Alice (2018): Paleoceanographic and climatic implications of a new Mediterranean Outflow branch in the southern Gulf of Cadiz. Quaternary Science Reviews, 197, 92-111, https://doi.org/10.1016/j.quascirev.2018.07.036 https://doi.pangaea.de/10.1594/PANGAEA.966840 https://doi.org/10.1594/PANGAEA.966840 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess AGE contourites Counting >150 µm fraction DEPTH sediment/rock Foraminifera planktic polar subpolar subtropical transitional GC Globorotalia scitula Gravity corer Gulf of Cadiz Heinrich Event 1 Hespérides Mediterranean outflow MOW MVSEIS08_TG-2 MVSEIS2008 Neogloboquadrina pachyderma sinistral sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas dataset 2024 ftpangaea https://doi.org/10.1594/PANGAEA.96684010.1594/PANGAEA.96660610.1016/j.quascirev.2018.07.036 2024-07-24T02:31:43Z For planktonic foraminifera counts, 9–12 cc of 68 bulk sub-samples were wet-weighed, freeze-dried, and re-weighed, then ultra-sonicated in a water bath, washed and sieved with tap and distilled water at the end through two grain-size fractions (63–150 μm and >150 μm) at the IGME. These fractions were dried on paper filters in the oven at 40 °C and weighed. Samples in the fraction >150 μm were split into adequate aliquots of at least 300–400 individuals for planktonic foraminifera census. The identification of species follows the taxonomy of Loeblich and Tappan (1964). Biogenic groups other than foraminifera and detrital minerals were counted in the same sample split. To trace the temperature of the surface water masses, planktonic foraminifera species were counted and classified into four assemblages, following the studies in the area (Bé and Tolderlund, 1971; Hemleben et al., 1989; Kucera, 2007; Reguera, 2001, 2004): polar (Neogloboquadrina pachyderma), subpolar (Neogloboquadrina incompta, Neogloboquadrina pachyderma-dutertrei, Neogloboquadrina dutertrei, Globigerina bulloides, Turborotalita quinqueloba), transitional (Globorotalia uvula, Globorotalia scitula, Globorotalia glutinata, Globorotalia inflata, Orbulina universa, Globorotalia truncatulinoides, Globorotalia hirsuta) and subtropical (Globigerinoides ruber-white, Globigerinoides ruber-pink, Globorotalia crassaformis, Globorotalia aequilateralis, Globigerina rubescens, Globigerina falconensis, Globigerinoides trilobus, Globigerinoides sacculifer). Dataset Neogloboquadrina pachyderma Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-6.841170,-6.841170,34.971330,34.971330) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AGE contourites Counting >150 µm fraction DEPTH sediment/rock Foraminifera planktic polar subpolar subtropical transitional GC Globorotalia scitula Gravity corer Gulf of Cadiz Heinrich Event 1 Hespérides Mediterranean outflow MOW MVSEIS08_TG-2 MVSEIS2008 Neogloboquadrina pachyderma sinistral sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas |
spellingShingle |
AGE contourites Counting >150 µm fraction DEPTH sediment/rock Foraminifera planktic polar subpolar subtropical transitional GC Globorotalia scitula Gravity corer Gulf of Cadiz Heinrich Event 1 Hespérides Mediterranean outflow MOW MVSEIS08_TG-2 MVSEIS2008 Neogloboquadrina pachyderma sinistral sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz |
topic_facet |
AGE contourites Counting >150 µm fraction DEPTH sediment/rock Foraminifera planktic polar subpolar subtropical transitional GC Globorotalia scitula Gravity corer Gulf of Cadiz Heinrich Event 1 Hespérides Mediterranean outflow MOW MVSEIS08_TG-2 MVSEIS2008 Neogloboquadrina pachyderma sinistral sortable silt SST (foraminifera) stable oxygen and carbon isotopes Younger Dryas |
description |
For planktonic foraminifera counts, 9–12 cc of 68 bulk sub-samples were wet-weighed, freeze-dried, and re-weighed, then ultra-sonicated in a water bath, washed and sieved with tap and distilled water at the end through two grain-size fractions (63–150 μm and >150 μm) at the IGME. These fractions were dried on paper filters in the oven at 40 °C and weighed. Samples in the fraction >150 μm were split into adequate aliquots of at least 300–400 individuals for planktonic foraminifera census. The identification of species follows the taxonomy of Loeblich and Tappan (1964). Biogenic groups other than foraminifera and detrital minerals were counted in the same sample split. To trace the temperature of the surface water masses, planktonic foraminifera species were counted and classified into four assemblages, following the studies in the area (Bé and Tolderlund, 1971; Hemleben et al., 1989; Kucera, 2007; Reguera, 2001, 2004): polar (Neogloboquadrina pachyderma), subpolar (Neogloboquadrina incompta, Neogloboquadrina pachyderma-dutertrei, Neogloboquadrina dutertrei, Globigerina bulloides, Turborotalita quinqueloba), transitional (Globorotalia uvula, Globorotalia scitula, Globorotalia glutinata, Globorotalia inflata, Orbulina universa, Globorotalia truncatulinoides, Globorotalia hirsuta) and subtropical (Globigerinoides ruber-white, Globigerinoides ruber-pink, Globorotalia crassaformis, Globorotalia aequilateralis, Globigerina rubescens, Globigerina falconensis, Globigerinoides trilobus, Globigerinoides sacculifer). |
format |
Dataset |
author |
Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel |
author_facet |
Lebreiro, Susana Martin Antón López, Laura Reguera, Maria Isabel |
author_sort |
Lebreiro, Susana Martin |
title |
Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz |
title_short |
Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz |
title_full |
Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz |
title_fullStr |
Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz |
title_full_unstemmed |
Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz |
title_sort |
climate associations of planktic foraminifera of sediment core mvseis08_tg-2 from gulf of cadiz |
publisher |
PANGAEA |
publishDate |
2024 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.966840 https://doi.org/10.1594/PANGAEA.966840 |
op_coverage |
LATITUDE: 34.971330 * LONGITUDE: -6.841170 * MINIMUM DEPTH, sediment/rock: 0.010 m * MAXIMUM DEPTH, sediment/rock: 2.125 m |
long_lat |
ENVELOPE(-6.841170,-6.841170,34.971330,34.971330) |
genre |
Neogloboquadrina pachyderma Planktonic foraminifera |
genre_facet |
Neogloboquadrina pachyderma Planktonic foraminifera |
op_relation |
https://doi.org/10.1594/PANGAEA.966606 Lebreiro, Susana Martin; Antón López, Laura; Reguera, Maria Isabel; Marzocchi, Alice (2018): Paleoceanographic and climatic implications of a new Mediterranean Outflow branch in the southern Gulf of Cadiz. Quaternary Science Reviews, 197, 92-111, https://doi.org/10.1016/j.quascirev.2018.07.036 https://doi.pangaea.de/10.1594/PANGAEA.966840 https://doi.org/10.1594/PANGAEA.966840 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.96684010.1594/PANGAEA.96660610.1016/j.quascirev.2018.07.036 |
_version_ |
1810457659803959296 |