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  • 1
    Publication Date: 2022-11-25
    Description: Abstract
    Description: We provide a globally distributed compilation of published surface temperature proxies for eight Cenozoic time periods that cover the range of paleoclimate states. The proxies have both a marine and terrestrial provenance and are compared to the annual temperature of the same location today. This data is then used to quantify long-term temperature changes on zonal and global levels. When coupled with recent estimates of atmospheric CO2 concentration, temperature data constrains the sensitivity of Earth's climate system to perturbation of the radiative balance, with possible implications for the future response to anthropogenic forcing. The dataset consists of an excel file with eight sheets for the eight selected timeslices, namely, •mid-Pliocene (3,0 - 3,3 Ma) •late Miocene (7,2 - 11,6 Ma) •mid-Miocene (14,7 - 17,0 Ma) •early Miocene (20,3 - 23,0 Ma) •early Oligocene (27,8 - 33,9 Ma) •late Eocene (33,9 - 37,8 Ma) •middle Eocene (42 - 46 Ma) •early Eocene (48 - 55 Ma)
    Description: Methods
    Description: Most data were directly adopted from the primary sources. However, a number of published datasets were recalculated from the published geochemical proxy indices using the recent Bayesian core-top calibrations BAYSPAR (Tierney & Tingley, 2015), BAYSPLINE (Tierney & Tingley, 2018), BAYFOX (Malevich et al., 2019), BAYMAG (Tierney et al., 2019) and BAYMBT (Crampton-Flood et al., 2020). These are highlighted in blue in the dataset. When more than one datapoint of a proxy is available for a given location, for example as part of a sea-surface temperature timeseries, then all datapoints falling within the bounds of our study timeslices were considered and the median was reported. Locations that are separated by less than 0.1 degrees in latitude and longitude were counted as a single locality.
    Keywords: lipid biomarkers ; coexistence approach ; leaf margin analysis ; microfossil assemblages ; oxygen isotopes ; bioclimatic analysis ; Earth system sensitivity ; Cenozoic ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC RADIATION 〉 RADIATIVE FORCING ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC TEMPERATURE 〉 TEMPERATURE ANOMALIES ; EARTH SCIENCE 〉 OCEANS 〉 OCEAN TEMPERATURE 〉 SEA SURFACE TEMPERATURE ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 LAND RECORDS 〉 PALEOVEGETATION ; EARTH SCIENCE 〉 PALEOCLIMATE 〉 PALEOCLIMATE RECONSTRUCTIONS 〉 AIR TEMPERATURE RECONSTRUCTION
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-01-02
    Description: Abstract
    Description: This dataset includes the first order (global) distribution of frost cracking intensities (FCI) [°C m], for selected paleoclimate time-slices during Late Cenozoic, as presented in the paper by Sharma et al. (2022). The paleoclimate time-slices correspond to Pre-Industrial (~1850 CE, PI), Mid-Holocene (~6 ka, MH), Last Glacial Maximum (~21 ka, LGM) and Pliocene (~3 Ma, PLIO). The FCI (by segregation ice growth) is predicted using the approach of Andersen et al. (2015), as a function of subsurface thermal gradient and volume of (and distance to) liquid water. The paleo-temperature reconstructions are obtained from ECHAM5 general circulation model (GCM) at T159 spatial resolution (80 km * 80 km) by Mutz et al. (2018). The spatial resolution of FCI dataset is same as ECHAM5 GCM simulations (i.e. 80 km * 80 km). The dataset comprises the following: -Scripts (Python) for modeling FCI for approach described in Sharma et al. (2022). -Global FCI distribution as netCDF and ascii formats. The data is available in both netCDF and ascii formats. However, the model code (attached Python scripts) currently supports only netCDF format. The model scripts can be freely utilized for regional and local studies which require finer resolution dataset. Please refer to the associated data description file for a detailed description of the dataset.
    Description: Methods
    Description: The model is based on the approach of Andersen et al. (2015) to estimate FCI as a function of subsurface thermal gradients up to the depth of 20 m. For segregation ice growth, it additionally considers the influence of volume of water available in the proximity of an ice lens. The boundary condition includes the presence of positive temperatures (T 〉 0 °C) at either boundary (at surface or 20 m depth). The frost cracking is supported if the bedrock temperature is in the frost cracking window (–8 °C and –3 °C). The integrated FCI each grid cell, across Earth’s terrestrial surface was calculated by depth integration of the FCI averaged over a period of 1 year. The unit of FCI data is °C m.
    Keywords: Periglacial processes ; frost weathering ; frost cracking intensity ; paleoclimate ; Cenozoic ; EarthShape ; EARTH SCIENCE 〉 SOLID EARTH 〉 GEOMORPHIC LANDFORMS/PROCESSES 〉 GLACIAL PROCESSES 〉 PERIGLACIAL PROCESSES
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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