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Journal articles on the topic 'Invertebrate archaeology'

Author: Grafiati

Published: 4 June 2021

Last updated: 18 February 2022

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1

Bourgeois-Roy, Andréanne, Hugo Crites, Pascal Bernatchez, Denis Lacelle, and André Martel. "Abrupt mortality of marine invertebrates at the Younger Dryas-Holocene transition in a shallow inlet of the Goldthwait Sea." Holocene 28, no. 12 (2018): 1894–908. http://dx.doi.org/10.1177/0959683618798130.

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The late Pleistocene–early Holocene transition period was characterized by rapid environmental change. Here, we investigate the impact of these changes on the marine invertebrates living in a shallow inlet of the post-glacial Goldthwait Sea. The site is located near Baie-Comeau (QC, Canada), where a number of remarkably well-preserved shell deposits are found along the Rivière aux Anglais Valley on the north shore of the St. Lawrence maritime estuary. Seven phyla of marine invertebrates with a minimum of 25 species or taxa were inventoried in a shell deposit, dominated by a community of Hiatel

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2

Keegan, William F., Roger W. Portell, and John Slapcinsky. "Changes in invertebrate taxa at two pre-Columbian sites in southwestern Jamaica, AD 800–1500." Journal of Archaeological Science 30, no. 12 (2003): 1607–17. http://dx.doi.org/10.1016/s0305-4403(03)00062-1.

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3

Miller, Randall F. "Location of trace fossils and problematica of George Frederic Matthew from Part W, Treatise on Invertebrate Paleontology." Journal of Paleontology 70, no. 1 (1996): 169–71. http://dx.doi.org/10.1017/s0022336000023210.

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George frederic matthew studied the geology of eastern Canada during the late 1800's to early 1900's and became an authority on Cambrian paleontology. Matthew advised the Geological Survey of Canada as its Cambrian expert and published over 200 papers spanning topics from Precambrian stromatolites to Pennsylvanian arthropods to archaeology (Miller, 1988a; Landing and Miller, 1988). He described a number of trace fossils and problematica cited in Hantzschel (1975), but the location of some specimens and their status has been uncertain, sometimes considered missing. Most of the specimens have no

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4

Faulkner, Patrick, Matthew Harris, Othman Haji, et al. "Long-term Trends in Terrestrial and Marine Invertebrate Exploitation on the Eastern African Coast: Insights from Kuumbi Cave, Zanzibar." Journal of Island and Coastal Archaeology 14, no. 4 (2018): 479–514. http://dx.doi.org/10.1080/15564894.2018.1501442.

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5

Ursenbacher, Stefan, Tabea Stötter, and Oliver Heiri. "Chitinous aquatic invertebrate assemblages in Quaternary lake sediments as indicators of past deepwater oxygen concentration." Quaternary Science Reviews 231 (March 2020): 106203. http://dx.doi.org/10.1016/j.quascirev.2020.106203.

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6

Serrand, Nathalie, and Dominique Bonnissent. "Interacting Pre-Columbian Amerindian Societies and Environments: Insights from Five Millennia of Archaeological Invertebrate Record on the Saint-Martin Island (French Lesser Antilles)." Environmental Archaeology 26, no. 1 (2018): 99–114. http://dx.doi.org/10.1080/14614103.2018.1450463.

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7

van Hardenbroek, Maarten, Päivi Rinta, Matthew J. Wooller, Jos Schilder, Tabea Stötter та Oliver Heiri. "Flotsam samples can help explain the δ13C and δ15N values of invertebrate resting stages in lake sediment". Quaternary Science Reviews 189 (червень 2018): 187–96. http://dx.doi.org/10.1016/j.quascirev.2018.04.008.

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8

van Hardenbroek, M., O. Heiri, F. J. W. Parmentier та ін. "Evidence for past variations in methane availability in a Siberian thermokarst lake based on δ13C of chitinous invertebrate remains". Quaternary Science Reviews 66 (квітень 2013): 74–84. http://dx.doi.org/10.1016/j.quascirev.2012.04.009.

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9

Rodrigues, Cyril G. "Successions of invertebrate microfossils and the late quaternary deglaciation of the central St Lawrence Lowland, Canada and United States." Quaternary Science Reviews 11, no. 5 (1992): 503–34. http://dx.doi.org/10.1016/0277-3791(92)90010-6.

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10

Vater, Amber E., and John A. Matthews. "Testing the ‘addition and persistence model’ of invertebrate succession in a subalpine glacier-foreland chronosequence: Fåbergstølsbreen, southern Norway." Holocene 23, no. 8 (2013): 1151–62. http://dx.doi.org/10.1177/0959683613483623.

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11

Brenskelle, Laura, Michelle LeFebvre, Rob Guralnick, et al. "Identifiers as Mechanisms for Linking Archaeological Data across Repositories." Biodiversity Information Science and Standards 2 (May 21, 2018): e26471. http://dx.doi.org/10.3897/biss.2.26471.

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Zooarchaeological specimens are the remains of animals, including vertebrate and invertebrate taxa, recovered from, or in association with, archaeological contexts of deposition or surrounding landscapes. The physical scope of zooarchaeological specimens is diverse and includes macro- and micro-zooarchaeological specimens composed of archaeologically preserved bone, shell, exoskeletons, teeth, hair or fur, scales, horns or antlers, as well as geochemical (e.g., isotopes) and biochemical (e.g., ancient DNA) signatures derived from faunal remains. Artifacts and objects created from animal remain

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12

Burleigh, Richard. "Decorative and Symbolic Uses of Fossils. Selected Groups, mainly Invertebrate. By Kenneth Oakley. 24.5 × 19 cm. Pp. xi+99, 49 figs. + 8 pls. Oxford: Pitt Rivers Museum, University of Oxford (Occasional Papers on Technology, 13), 1985. ISBN 0-902793-17-9. £8.95 (p/b)." Antiquaries Journal 67, no. 2 (1987): 392–93. http://dx.doi.org/10.1017/s0003581500025531.

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13

Hannon, Gina E., Karen Halsall, Chiara Molinari, John Boyle, and Richard HW Bradshaw. "The reconstruction of past forest dynamics over the last 13,500 years in SW Sweden." Holocene 28, no. 11 (2018): 1791–800. http://dx.doi.org/10.1177/0959683618788669.

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Evidence for unbroken continuity of tree taxa over the last c. 13,500 years is presented from a biodiversity ‘hotspot’ nature reserve in south-west Sweden. Forest composition, continuity, fire and disturbance events are reconstructed using palaeoecological methods. A lake record reveals that Pinus sylvestris, Betula spp., Salix spp., Populus tremula and Hippophae rhamnoides were the initial trees scattered in a semi-open, steppe environment. This developed into forest with Pinus, Betula, Corylus, Alnus, Ulmus and Populus with evidence for frequent fires. Deciduous trees became more significant

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14

McCobb, L. M. E., D. E. G. Briggs, A. R. Hall, and H. K. Kenward. "The Preservation of Invertebrates in 16th-Century Cesspits at St Saviourgate, York*." Archaeometry 46, no. 1 (2004): 157–69. http://dx.doi.org/10.1111/j.1475-4754.2004.00150.x.

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15

Benayas, J., L. Pertierra, P. Tejedo, et al. "A review of scientific research trends within ASPA No. 126 Byers Peninsula, South Shetland Islands, Antarctica." Antarctic Science 25, no. 2 (2013): 128–45. http://dx.doi.org/10.1017/s0954102012001058.

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AbstractByers Peninsula, Livingston Island, was one of the first sites in Antarctica designated for environmental conservation and scientific protection. Research on Byers Peninsula has been predominantly international, with 88 indexed publications (93% of them published during last 20 years) from 209 authors affiliated to 110 institutions from 22 nations, all of which are signatories to the Antarctic Treaty. Palaeontological research represented 20% of the published articles. The variety of freshwater bodies within the area has made Byers Peninsula a reference site for limnological studies (2

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16

Creamer, Winifred, Jonathan Haas, Edward Jakaitis, and Jesus Holguin. "Far From the Shore: Comparison of Marine Invertebrates in Midden Deposits From Two Sites in the Norte Chico, Peru." Journal of Island and Coastal Archaeology 6, no. 2 (2011): 176–95. http://dx.doi.org/10.1080/15564894.2011.582071.

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17

Whitaker, Adrian R. "Incipient aquaculture in prehistoric California?: Long-term productivity and sustainability vs. immediate returns for the harvest of marine invertebrates." Journal of Archaeological Science 35, no. 4 (2008): 1114–23. http://dx.doi.org/10.1016/j.jas.2007.08.005.

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18

Berman, Daniil, Arcady Alfimov, and Svetlana Kuzmina. "Invertebrates of the relict steppe ecosystems of Beringia, and the reconstruction of Pleistocene landscapes." Quaternary Science Reviews 30, no. 17-18 (2011): 2200–2219. http://dx.doi.org/10.1016/j.quascirev.2010.09.016.

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19

Gowlett, J. A. J. "The discovery of fire by humans: a long and convoluted process." Philosophical Transactions of the Royal Society B: Biological Sciences 371, no. 1696 (2016): 20150164. http://dx.doi.org/10.1098/rstb.2015.0164.

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Numbers of animal species react to the natural phenomenon of fire, but only humans have learnt to control it and to make it at will. Natural fires caused overwhelmingly by lightning are highly evident on many landscapes. Birds such as hawks, and some other predators, are alert to opportunities to catch animals including invertebrates disturbed by such fires and similar benefits are likely to underlie the first human involvements with fires. Early hominins would undoubtedly have been aware of such fires, as are savanna chimpanzees in the present. Rather than as an event, the discovery of fire u

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20

Ascough, P. L., G. T. Cook, M. J. Church, et al. "Temporal and Spatial Variations in Freshwater 14C Reservoir Effects: Lake Mývatn, Northern Iceland." Radiocarbon 52, no. 3 (2010): 1098–112. http://dx.doi.org/10.1017/s003382220004618x.

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Lake Mývatn is an interior highland lake in northern Iceland that forms a unique ecosystem of international scientific importance and is surrounded by a landscape rich in archaeological and paleoenvironmental sites. A significant freshwater reservoir effect (FRE) has been identified in carbon from the lake at some Viking (about AD 870–1000) archaeological sites in the wider region (Mývatnssveit). Previous accelerator mass spectrometry (AMS) measurements indicated this FRE was about 1500–1900 14C yr. Here, we present the results of a study using stable isotope and 14C measurements to quantify t

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21

Moss, Madonna L. "Did Tlingit Ancestors Eat Sea Otters? Addressing Intellectual Property and Cultural Heritage through Zooarchaeology." American Antiquity 85, no. 2 (2020): 202–21. http://dx.doi.org/10.1017/aaq.2019.101.

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The maritime fur trade caused the extirpation of sea otters from southeast Alaska. In the 1960s, sea otters were reintroduced, and their numbers have increased. Now, sea otters are competing with people for what have become commercially important invertebrates. After having been absent for more than a century, the reentry of this keystone species has unsettled people. Although some communities perceive sea otters as a threat to their livelihoods, others view their return as restoration of the marine ecosystem. The federal Marine Mammal Protection Act authorizes any Alaska Native to harvest sea

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22

Bhiry, Najat, Armelle Decaulne, and Myosotis Bourgon-Desroches. "Development of a subarctic peatland linked to slope dynamics at Lac Wiyâshâkimî (Nunavik, Canada)." Holocene 29, no. 9 (2019): 1459–67. http://dx.doi.org/10.1177/0959683619854516.

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A palaeoecological study of a subarctic minerotrophic peatland was undertaken to reconstruct the formation of the site as an archive of slope geomorphological processes. The study peatland is located about 400 m from Caribou slope (unofficial name) on Lepage Island, Lac Wiyâshâkimî, Nunavik (northern Québec, Canada). The site is close to the lakeshore and receives runoff directly from Caribou slope and its catchment. Gravity processes have been active on Caribou slope since the deglaciation of the region at approximately 6000 cal. yr BP. These processes may be differentiated in terms of Holoce

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23

López-Dóriga, Inés. "Mineralised plant and invertebrate remains: a guide to the identification of calcium phosphate replaced remains." Archaeological Journal, April 6, 2021, 1–2. http://dx.doi.org/10.1080/00665983.2021.1894758.

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24

Rautenbach, J. C. "Third cumulative index for Koedoe: volumes 35/2-44/1." Koedoe 44, no. 2 (2001). http://dx.doi.org/10.4102/koedoe.v44i2.179.

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Index to Koedoe: volumes 35/2 - 44/1 Authors85 Subjects98 Botany 98 Ecology and behaviour 100 Wildlife conservation & techniques 100 Zoology102 Invertebrata 102 Pisces 103 Amphibia 103 Reptilia 103 Aves104 Mammalia 104 Archaeology and History 105 Bibliography 106 Climate 106 Geologyand Pedology 106 Environmental impact on rivers & water quality 106 Check list 107 Issues in conservation 107 Maps 108 Social Science 108 Parks

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25

Hutterer, Rainer, Oskar Schröder, and Jörg Linstädter. "Food and Ornament: Use of Shellfish at Ifri Oudadane, a Holocene Settlement in NE Morocco." African Archaeological Review, October 9, 2020. http://dx.doi.org/10.1007/s10437-020-09409-3.

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Abstract Recent excavations of Ifri Oudadane, a prehistoric rockshelter on the Mediterranean coast of NW Morocco, yielded a rich marine and terrestrial fauna. We present an analysis of the shellfish remains (exoskeleton-bearing aquatic invertebrates) from the 2011 trench, covering the Epipaleolithic and Early Neolithic levels. A total of 4,415 liters of sediment contained 8,749 specimens (MNI) of at least 40 species of shellfish: 12 bivalves, 24 gastropods, one tusk shell, barnacles, crabs, and sea urchins. The mean abundance of shellfish was 2 MNI per liter. Limpets (Patellidae), topshells (T

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26

Shumilovskikh, Lyudmila S., Elena S. Shumilovskikh, Frank Schlütz, and Bas van Geel. "NPP-ID: Non-Pollen Palynomorph Image Database as a research and educational platform." Vegetation History and Archaeobotany, August 30, 2021. http://dx.doi.org/10.1007/s00334-021-00849-8.

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AbstractNon-pollen palynomorphs (NPPs) form a large group of biological objects found in palynological slides besides pollen grains. This includes various remains of algae and fungi, shells, resting stages and eggs of invertebrates, among others. Publications of NPP-types started in the 1970s with studies of BvG and colleagues, and large numbers of new types continue to be published every year. For an overview of this diverse world of “extra fossils”, we created the Non-Pollen Palynomorph Image Database (NPP-ID) to gather NPP knowledge, structured by acronyms and known taxonomy to assist ident

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