Past and ongoing human activities have shaped the geographical ranges and diversity of species. New genomic techniques applied to degraded samples, such as those from natural history collections, can uncover the complex evolutionary consequences of human pressures and generate baselines for interpreting magnitudes of species loss or persistence relevant to conservation. Here we integrate mitogenomic data with historical records from a recently rediscovered Bahamian hutia (; (FMP Z02816)) specimen at the Fairbanks Museum & Planetarium (Vermont, USA) to determine when and where the specimen was collected and to place it in a phylogenetic context with specimens that both predate (palaeontological) and postdate (archaeological) human arrival in The Bahamas. We determined that this specimen was part of the same population as the named holotype specimen in 1891 on East Plana Cay (EPC). Bahamian hutia populations were widely extirpated following European colonization. Today, EPC hosts the last remaining natural Bahamian hutia population. Mitogenomic data places the focal specimen within the southern Bahamian hutia population, which is now largely restricted to EPC. The results reveal previously undocumented genetic continuity among the EPC population for at least the past 500 years, highlighting how 'dark' museum specimens inform new conservation-relevant understandings of diversity.
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http://dx.doi.org/10.1098/rsbl.2022.0566 | DOI Listing |
Biol Lett
April 2023
Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA.
Past and ongoing human activities have shaped the geographical ranges and diversity of species. New genomic techniques applied to degraded samples, such as those from natural history collections, can uncover the complex evolutionary consequences of human pressures and generate baselines for interpreting magnitudes of species loss or persistence relevant to conservation. Here we integrate mitogenomic data with historical records from a recently rediscovered Bahamian hutia (; (FMP Z02816)) specimen at the Fairbanks Museum & Planetarium (Vermont, USA) to determine when and where the specimen was collected and to place it in a phylogenetic context with specimens that both predate (palaeontological) and postdate (archaeological) human arrival in The Bahamas.
View Article and Find Full Text PDFSci Rep
January 2020
Florida Museum of Natural History, University of Florida, Gainesville, FL, 32611, USA.
Quaternary paleontological and archaeological evidence often is crucial for uncovering the historical mechanisms shaping modern diversity and distributions. We take an interdisciplinary approach using multiple lines of evidence to understand how past human activity has shaped long-term animal diversity in an island system. Islands afford unique opportunities for such studies given their robust fossil and archaeological records.
View Article and Find Full Text PDFPLoS One
March 2020
Department of Anthropology, University of Florida, Gainesville, Florida, United States of America.
Bahamian hutias (Geocapromys ingrahami) are the only endemic terrestrial mammal in The Bahamas and are currently classified as a vulnerable species. Drawing on zooarchaeological and new geochemical datasets, this study investigates human management of Bahamian hutias as cultural practice at indigenous Lucayan settlements in The Bahamas and the Turks & Caicos Islands. In order to determine how hutia diet and distribution together were influenced by Lucayan groups we conducted isotopic analysis on native hutia bone and tooth enamel recovered at the Major's Landing site on Crooked Island in The Bahamas and introduced hutias from the Palmetto Junction site on Providenciales in the Turks & Caicos Islands.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
December 2007
Florida Museum of Natural History, University of Florida, P.O. Box 117800, Gainesville, FL 32611, USA.
We report Quaternary vertebrate and plant fossils from Sawmill Sink, a "blue hole" (a water-filled sinkhole) on Great Abaco Island, The Bahamas. The fossils are well preserved because of deposition in anoxic salt water. Vertebrate fossils from peat on the talus cone are radiocarbon-dated from approximately 4,200 to 1,000 cal BP (Late Holocene).
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