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Physical properties of sediment cores TG-03, Ona Basin, southwestern Scotia S...
During expedition SCAN 2013, gravity core TG-03 was collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. The core is 295 cm long and... -
Physical properties of sediment cores TG-01, Ona Basin, southwestern Scotia S...
During expedition SCAN 2013, gravity core TG-01 was collected in the Ona High slope, central Ona Basin, NE prolongation of the Antarctic Peninsula. The core is 400 cm long and... -
Relative abundance of pollen and spores in a sediment core from Lake Pacú, lo...
This dataset presents the relative abundance of pollen and spores from 68 sediment samples collected at 0.10 m intervals along core NGR07, retrieved from Lake Pacú in the lower... -
Relative abundance of diatoms in a sediment core from Lake Pacú, lower Negro ...
This dataset contains the relative abundance of diatom taxa identified in 68 sediment samples collected at 0.10 m intervals from core NGR07, from Lake Pacú, in the lower Negro... -
Uranium-Thorium analysis from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Silica weight percent from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Nitrogen weight percent from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Diatom abundance from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Age model data from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Diatom assemblage of the sediment short core EN18232-1, Lake Khamra, Siberia
This data set is an extension to the previously published data in a bundled publication (Stieg et al., 2024a) from the Russian Lake Khamra (59.99°N, 112.98°E, 340 m a.s.l.),... -
Accumulation rates from sediment core 16-KP-04-L19B, Lake Rauchuagytgyn, expe...
These dataset contains multi proxy data from short sediment core 16-KP-04-L19B obtained from Arctic glacial lake Rauchuagytgyn (N 67.7888, E 168.7380) by gravity coring during... -
Diatom species from sediment core 16-KP-04-L19B, Lake Rauchuagytgyn, expediti...
These dataset contains multi proxy data from short sediment core 16-KP-04-L19B obtained from Arctic glacial lake Rauchuagytgyn (N 67.7888, E 168.7380) by gravity coring during... -
Accumulation rates from sediment core EN18218, Lake Rauchuagytgyn, expedition...
These dataset contains multi proxy data from sediment core EN18218 obtained from Arctic glacial lake Rauchuagytgyn (67.7922°N, 168.7312°E) by piston coring during the Chukotka... -
Diatom species from sediment core EN18218, Lake Rauchuagytgyn, expedition to ...
These dataset contains multi proxy data from sediment core EN18218 obtained from Arctic glacial lake Rauchuagytgyn (67.7922°N, 168.7312°E) by piston coring during the Chukotka... -
Intra- and interannual patterns of diatom population occurrence in the Maurit...
Qualitative and quantitative analyses of the diatom community were carried out on permanent slides of acid cleaned material (Mountex® mounting medium) at x1000 magnifications by... -
MIS 5e Southern Ocean September sea-ice concentrations and summer sea-surface...
Marine Isotope Stage (MIS) 5e is the latest period when global atmospheric temperatures were warmer than present and global sea levels were higher than present. Environmental... -
Silicon isotopes from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Radiocarbon ages from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Diatom assemblages determined by differential phase interference microscopy o...
The Iberian Margin, located in the North Atlantic mid-latitudes at the western edge of the European continent, is a crucial areafor climate and oceanographic reconstructions. As... -
Diatom assemblages and biogenic silica from IODP Site 383-U1539
From the complete downcore record of IODP Site 383-U1539, sampling was conducted at 1 m resolution. Quantitative diatom slides were prepared following the settling method of...
