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75 results for “Last Glacial Maximum”
Low sea surface salinity event of the Japan Sea during the Last Glacial Maximum
<p>The data and code for MIROC4m (also contains PMIP3) simulation results for "Low sea surface salinity event of the Japan Sea during the Last Glacial Maximum".</p>
Fig. 4 in First record of North Italian roach, Leucos aula (Bonaparte, 1841) on the Pag Island, Croatia-relict of the last glacial maximum?
Fig. 4 Leucos aula (left lateral view) a HDBI 1525, Pag Island, Velo Blato, SL 70.1 mm, b NMW50699, Karin, SL 74.9 mm, and c NMW 84,857, Lago Campagna, Torino Prov., SL 65.9 mm
Data from: Lizards on ice: evidence for multiple refugia in Liolaemus pictus (Liolaemidae) during the Last Glacial Maximum in the southern Andean beech forests
Historical climate changes and orogenesis are two important factors that have shaped intraspecific biodiversity patterns worldwide. Although southern South America has experienced such complex events, there is a paucity of studies examining the effects on intraspecific diversification in this part of the world. Liolaemus pictus is the southernmost distributed lizard in the Chilean temperate forest, whose genetic structure has likely been influenced by Pleistocene glaciations. We conducted a phylogeographic study of L. pictus in Chile and Argentina based on one mitochondrial and two nuclear genes, and recovered two strongly divergent groups, Northern and Southern clades, the former distributed from the northernmost limit of the species to the Araucanía region, and the latter being distributed throughout the Andes and the Chiloé archipelago in Southern Chile. Our results suggest that L. pictus originated 751 Kya, with divergence between the two clades occurring in the late Pleistocene. Demographic reconstructions for the Northern and Southern clades indicate a decrease in effective population sizes likely associated with Pleistocene glaciations. Surprisingly, patterns of genetic variation, clades ages and historical gene flow in populations distributed within the limits of the Last Glacial Maximum (LGM) are not explained by recent colonization. We propose an "intra-Andean multiple refuge" hypothesis, along with the classical refuge hypothesis previously proposed for the biota of the Chilean Coastal range and Eastern Andean Cordillera. Our hypothesis is supported by niche modeling analysis suggesting the persistence of fragments of suitable habitat for the species within the limits of the LGM ice shield. This type of refuge hypothesis is proposed for the first time for an ectothermic species.
Simulation outputs for the manuscript "Snowball Earth transitions from Last Glacial Maximum conditions provide an independent upper limit on Earth's climate sensitivity"
<p>This dataset contains outputs for the simulations shown in the paper "Snowball Earth transitions from Last Glacial Maximum conditions provide an independent upper limit on Earth’s climate sensitivity" by Renoult et al. (submitted). </p> <p>The outputs contain different 2D and 3D variables described in the paper and the file "README.txt".</p>
Assessment of equilibrium climate sensitivity of the Community Earth System Model version 2 through simulation of the Last Glacial Maximum
<p>Simulation data (TS, FSNT, and FLNT) and apap cloud feedback analysis for CESM2 LGM simulation</p> <p><strong>Simulation boundary condition files in 1-degree resolution: boundary_condition_files.zip</strong></p> <p><strong>Please cite: </strong></p> <p>Zhu, J., Otto-Bliesner, B. L., Brady, E. C., Poulsen, C. J., Tierney, J. E., Lofverstrom, M., & DiNezio, P. (2021). Assessment of equilibrium climate sensitivity of the Community Earth System Model version 2 through simulation of the Last Glacial Maximum. <em>Geophysical Research Letters</em>, <em>n/a</em>(n/a), e2020GL091220. https://doi.org/10.1029/2020GL091220</p>
Precipitation isotope changes over the East Asian monsoon region driven by sea surface temperature during the Last Glacial Maximum
<p>This dataset includes speleothem and ice core proxies used for paper [Lan et al., (2023): Precipitation isotope changes over the East Asian monsoon region driven by sea surface temperature during the Last Glacial Maximum].</p>
Data from: Phylogeography of Dendrolimus punctatus (Lepidoptera: Lasiocampidae): population differentiation and last glacial maximum survival
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Data from: Approximate Bayesian computation analysis of EST-associated microsatellites indicates that the broadleaved evergreen tree Castanopsis sieboldii survived the Last Glacial Maximum in multiple refugia in Japan
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Data from: Lizards on ice: evidence for multiple refugia in Liolaemus pictus (Liolaemidae) during the Last Glacial Maximum in the southern Andean beech forests
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Data from: Extinction debt and delayed colonization have had comparable but unique effects on plant community-climate lags since the Last Glacial Maximum
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Population collapse in viviparid gastropods of the Lake Victoria ecoregion started before the Last Glacial Maximum
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Climate and ice in the last glacial maximum explain patterns of isolation by distance inferred for alpine grasshoppers
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Data from: Last Glacial Maximum environmental conditions at Andøya, northern Norway; evidence for a northern ice-edge ecological “hotspot”
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Ice sheet effects to the Asian winter monsoon since the Last Glacial Maximum
<p><strong><em>Modern climate data, surface sediment dataset, <em><strong> Simu</strong></em>lations of TRACE and PMIP3.</em></strong></p>
A dataset of global lake-level simulations and reconstructions since the Last Glacial Maximum
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Geothermal heating affecting ocean stratification and circulation after the Last Glacial Maximum
<p>Data generated in this study is archived here.</p>
Figures 6-10 from: Sendra A, Wagnell C (2019) The cave-dwelling dipluran (Diplura, Campodeidae) on the edge of the Last Glacial Maximum in Vancouver Island caves, North America (Canada). Subterranean Biology 29: 59-77. https://doi.org/10.3897/subtbiol.29.31467
Figures 6-10 Haplocampawagnelli Sendra, sp. n. 6 distal gouge sensilla whorl in a medial antennomere 7 medial antennomere 8 detail of the ending portion of a gouge sensillum 9 detail of external side of a gouge sensillum 10 detail of lateral side of a gouge sensillum.
Supplementary material 1 from: Sendra A, Wagnell C (2019) The cave-dwelling dipluran (Diplura, Campodeidae) on the edge of the Last Glacial Maximum in Vancouver Island caves, North America (Canada). Subterranean Biology 29: 59-77. https://doi.org/10.3897/subtbiol.29.31467
: Data type: multimedia
Figures 29-33 from: Sendra A, Wagnell C (2019) The cave-dwelling dipluran (Diplura, Campodeidae) on the edge of the Last Glacial Maximum in Vancouver Island caves, North America (Canada). Subterranean Biology 29: 59-77. https://doi.org/10.3897/subtbiol.29.31467
Figures 29-33 29 Map of Fossli Slots caves with spots where Haplocampawagnelli sp. n. was seen 30 entrance of Fossli Slot #2 cave 31 Kiku Pot cave with spots where Haplocampawagnelli sp. n. was seen 32 entrance of Kiku Pot cave with Felix Ossigi-Bonanno and Craig Wagnell after the success finding 33 entrance of Kiku Pot cave viewed from inside the cave.
Figures 1-5 from: Sendra A, Wagnell C (2019) The cave-dwelling dipluran (Diplura, Campodeidae) on the edge of the Last Glacial Maximum in Vancouver Island caves, North America (Canada). Subterranean Biology 29: 59-77. https://doi.org/10.3897/subtbiol.29.31467
Figures 1-5 Haplocampawagnelli Sendra, sp. n. 1 last and penultimate antennomere 2 olfactory chemoreceptors within the cupuliform organ 3 detail of olfactory chemoreceptor, paratype 4 coniform sensilla on the last antennomeres 5 two rosette sensilla in the last antennomere.
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OpenNeuro
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