T105 Fossil Specimens 0's and 1'??s: Databases, Standards, & Mobilization

Monday, 26 September 2016
8:00 AM - 12:00 PM
Mile High Ballroom 4C

PALEO-GEOREFERENCING AND DEEP TIME VIZUALIZATION OF LOCALITY DATA

Paper number: T105-13
Program: Technical Sessions
Time: 11:00 AM – 11:15 AM

Authors

Abstract

Georeferencing of localities is part of the digitization process for natural history collections. This effort covers both modern and geological specimens, and paves the way to potential deep time visualizations. Localities in modern geography are easily mapped using resources such as Google Earth© and digital topographic maps; add the time dimension, and the resources are more limited.

We have developed an open-source paleo location mapping service, paleolocation.org to provide that resource. A web service call is made by entering three parameters: age of the rock or fossil of interest, the latitude, and the longitude of its modern map location. The web service then returns a URL pointing to its location on the modern map and creates a second map indicating the location of the site where it would have been during the age entered. The response from paleolocation.org is based on reconstructions from the PLATES project of The University of Texas Institute for Geophysics. These reconstructions contain both the base map as well as the data required to perform the Euler rotations of the requested point on the modern globe to its location on the requested reconstruction. The specimen is mapped in deep geologic time.

This mapping ability is integrated into Paleocentral.org. The original allows us to query a static database of type specimens and plot onto a Google Earth© environment. The update version queries the complete Specify 6 database, provides a Google Earth© view, a geology map view, or a reconstruction of plates in deep time. The current geographical coordinates are stored within the database and link to objects collected from that site. The rotated coordinates are not stored. A collecting event concept is used to connect the deep time chrono-, litho-, or biostratigraphy for that particular event. The same geographic point can have multiple geological contexts. This is especially valuable for sections, cores, and core-sourced microfossils.

Geological Society of America Abstracts with Programs. Vol. 48, No. 7

doi: 10.1130/abs/2016AM-285999

© Copyright 2016 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.