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'''Dwarf elephants''' are prehistoric members of the order [[Proboscidea]] which, through the process of [[allopatric speciation]] on islands, evolved much smaller body sizes (around {{convert|1|-|2.3|m}} shoulder height) in comparison with their immediate ancestors. Dwarf elephants are an example of [[insular dwarfism]], the phenomenon whereby large terrestrial vertebrates (usually mammals) that colonize islands evolve dwarf forms, a phenomenon attributed to adaptation to resource-poor environments and lack of predation and competition. |
'''Dwarf elephants''' are prehistoric members of the order [[Proboscidea]] which, through the process of [[allopatric speciation]] on islands, evolved much smaller body sizes (around {{convert|1|-|2.3|m}} shoulder height) in comparison with their immediate ancestors. Dwarf elephants are an example of [[insular dwarfism]], the phenomenon whereby large terrestrial vertebrates (usually mammals) that colonize islands evolve dwarf forms, a phenomenon attributed to adaptation to resource-poor environments and lack of predation and competition. |
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[[Fossil]] remains of dwarf elephants have been found on the [[Mediterranean]] islands of [[Cyprus]], [[Malta]], [[Crete]] |
[[Fossil]] remains of dwarf elephants have been found on the [[Mediterranean]] islands of [[Cyprus]], [[Malta]], [[Crete]], [[Sicily]], [[Sardinia]], the [[Cyclades|Cyclades Islands]] and the [[Dodecanese Islands]], which are mostly members of the genus ''[[Palaeoloxodon]]'', descending from the large {{Convert|4|m|ft}} tall mainland European species ''[[Palaeoloxodon antiquus]],'' though two species represent dwarf mammoths. Dwarf species of elephants and ''[[Stegodon]]'' have been found on the islands of Indonesia and the Philippines, with dwarfed species of ''Stegodon'' also having been found in Japan. The [[Channel Islands (California)|Channel Islands of California]] once supported [[Mammuthus exilis|a dwarf species]] descended from [[Columbian mammoth]]s,<ref>{{cite web | url = https://www.nps.gov/chis/learn/historyculture/pygmymammoth.htm | title = The Pygmy Mammoth (U.S. National Park Service) }}</ref> while the [[woolly mammoth]]s that existed on [[Wrangel Island]] north of [[Siberia]] were once considered dwarfs, but are not anymore. |
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==The Mediterranean islands== |
==The Mediterranean islands== |
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Sicily and Malta were inhabited by two successive waves of dwarf elephants derived from ''P. antiquus,'' which first arrived on the islands at least 500,000 years ago. The first of these species is ''[[Palaeoloxodon falconeri|P. falconeri]] ,'' which is one of the smallest dwarf elephant species at around {{Convert|1|m|ft}} tall, and was strongly modified from its ancestor in numerous aspects, which lived in a depauperate fauna with no other large mammal species.''<ref name=":02">Bonfiglio, L., Marra, A. C., Masini, F., Pavia, M., & Petruso, D. (2002). [https://iris.unito.it/bitstream/2318/91517/1/18%20-%20Bonfiglio%20et%20al%202002%20Sicily%20A%20Review%20BAR.pdf Pleistocene faunas of Sicily: a review]. In W. H. Waldren, & J. A. Ensenyat (Eds.), ''World islands in prehistory: international insular investigations''. British Archaeological Reports, International Series, 1095, 428–436.</ref>''<ref name=":12">{{Cite journal |last=Scarborough |first=Matthew Edward |date=March 2022 |title=Extreme Body Size Variation in Pleistocene Dwarf Elephants from the Siculo-Maltese Palaeoarchipelago: Disentangling the Causes in Time and Space |journal=Quaternary |language=en |volume=5 |issue=1 |pages=17 |doi=10.3390/quat5010017 |issn=2571-550X |doi-access=free |hdl-access=free |hdl=11427/36354}}</ref> Later, around 200,000 years ago, this species was replaced by a second colonisation by ''P. antiquus'', which gave rise to the larger (though still considerably dwarfed) {{Convert|2|m|ft}} tall species ''[[Palaeoloxodon mnaidriensis|P. mnaidriensis]],'' which on Sicily lived alongside a number other large mammal species, including herbivores and carnivores.<ref name=":12" /><ref name=":3">{{Cite journal |last1=Baleka |first1=Sina |last2=Herridge |first2=Victoria L. |last3=Catalano |first3=Giulio |last4=Lister |first4=Adrian M. |last5=Dickinson |first5=Marc R. |last6=Di Patti |first6=Carolina |last7=Barlow |first7=Axel |last8=Penkman |first8=Kirsty E.H. |last9=Hofreiter |first9=Michael |last10=Paijmans |first10=Johanna L.A. |date=August 2021 |title=Estimating the dwarfing rate of an extinct Sicilian elephant |url=https://linkinghub.elsevier.com/retrieve/pii/S0960982221007351 |journal=Current Biology |language=en |volume=31 |issue=16 |pages=3606–3612.e7 |doi=10.1016/j.cub.2021.05.037 |pmid=34146486 |s2cid=235477150 |doi-access=free}}</ref><ref name=":122">{{Cite journal |last1=Bethune |first1=Elehna |last2=Kaiser |first2=Thomas M. |last3=Schulz-Kornas |first3=Ellen |last4=Winkler |first4=Daniela E. |date=November 2019 |title=Multiproxy dietary trait reconstruction in Pleistocene Hippopotamidae from the Mediterranean islands |url=https://zenodo.org/record/3248597 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=533 |pages=109210 |bibcode=2019PPP...533j9210B |doi=10.1016/j.palaeo.2019.05.032 |s2cid=181824675}}</ref> The youngest records of this species on Sicily date to around 20,000 years ago, close to the time of arrival of modern humans on Sicily.<ref name=":2">{{Cite journal |last1=Palombo |first1=Maria Rita |last2=Antonioli |first2=Fabrizio |last3=Di Patti |first3=Carolina |last4=Valeria |first4=Lo Presti |last5=Scarborough |first5=Matthew E. |date=2021-10-03 |title=Was the dwarfed Palaeoloxodon from Favignana Island the last endemic Pleistocene elephant from the western Mediterranean islands? |url=https://www.tandfonline.com/doi/full/10.1080/08912963.2020.1772251 |journal=Historical Biology |language=en |volume=33 |issue=10 |pages=2116–2134 |doi=10.1080/08912963.2020.1772251 |issn=0891-2963 |s2cid=225710152}}</ref> |
Sicily and Malta were inhabited by two successive waves of dwarf elephants derived from ''P. antiquus,'' which first arrived on the islands at least 500,000 years ago. The first of these species is ''[[Palaeoloxodon falconeri|P. falconeri]] ,'' which is one of the smallest dwarf elephant species at around {{Convert|1|m|ft}} tall, and was strongly modified from its ancestor in numerous aspects, which lived in a depauperate fauna with no other large mammal species.''<ref name=":02">Bonfiglio, L., Marra, A. C., Masini, F., Pavia, M., & Petruso, D. (2002). [https://iris.unito.it/bitstream/2318/91517/1/18%20-%20Bonfiglio%20et%20al%202002%20Sicily%20A%20Review%20BAR.pdf Pleistocene faunas of Sicily: a review]. In W. H. Waldren, & J. A. Ensenyat (Eds.), ''World islands in prehistory: international insular investigations''. British Archaeological Reports, International Series, 1095, 428–436.</ref>''<ref name=":12">{{Cite journal |last=Scarborough |first=Matthew Edward |date=March 2022 |title=Extreme Body Size Variation in Pleistocene Dwarf Elephants from the Siculo-Maltese Palaeoarchipelago: Disentangling the Causes in Time and Space |journal=Quaternary |language=en |volume=5 |issue=1 |pages=17 |doi=10.3390/quat5010017 |issn=2571-550X |doi-access=free |hdl-access=free |hdl=11427/36354}}</ref> Later, around 200,000 years ago, this species was replaced by a second colonisation by ''P. antiquus'', which gave rise to the larger (though still considerably dwarfed) {{Convert|2|m|ft}} tall species ''[[Palaeoloxodon mnaidriensis|P. mnaidriensis]],'' which on Sicily lived alongside a number other large mammal species, including herbivores and carnivores.<ref name=":12" /><ref name=":3">{{Cite journal |last1=Baleka |first1=Sina |last2=Herridge |first2=Victoria L. |last3=Catalano |first3=Giulio |last4=Lister |first4=Adrian M. |last5=Dickinson |first5=Marc R. |last6=Di Patti |first6=Carolina |last7=Barlow |first7=Axel |last8=Penkman |first8=Kirsty E.H. |last9=Hofreiter |first9=Michael |last10=Paijmans |first10=Johanna L.A. |date=August 2021 |title=Estimating the dwarfing rate of an extinct Sicilian elephant |url=https://linkinghub.elsevier.com/retrieve/pii/S0960982221007351 |journal=Current Biology |language=en |volume=31 |issue=16 |pages=3606–3612.e7 |doi=10.1016/j.cub.2021.05.037 |pmid=34146486 |s2cid=235477150 |doi-access=free}}</ref><ref name=":122">{{Cite journal |last1=Bethune |first1=Elehna |last2=Kaiser |first2=Thomas M. |last3=Schulz-Kornas |first3=Ellen |last4=Winkler |first4=Daniela E. |date=November 2019 |title=Multiproxy dietary trait reconstruction in Pleistocene Hippopotamidae from the Mediterranean islands |url=https://zenodo.org/record/3248597 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=533 |pages=109210 |bibcode=2019PPP...533j9210B |doi=10.1016/j.palaeo.2019.05.032 |s2cid=181824675}}</ref> The youngest records of this species on Sicily date to around 20,000 years ago, close to the time of arrival of modern humans on Sicily.<ref name=":2">{{Cite journal |last1=Palombo |first1=Maria Rita |last2=Antonioli |first2=Fabrizio |last3=Di Patti |first3=Carolina |last4=Valeria |first4=Lo Presti |last5=Scarborough |first5=Matthew E. |date=2021-10-03 |title=Was the dwarfed Palaeoloxodon from Favignana Island the last endemic Pleistocene elephant from the western Mediterranean islands? |url=https://www.tandfonline.com/doi/full/10.1080/08912963.2020.1772251 |journal=Historical Biology |language=en |volume=33 |issue=10 |pages=2116–2134 |doi=10.1080/08912963.2020.1772251 |issn=0891-2963 |s2cid=225710152}}</ref> |
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The dwarf mammoth species ''[[Mammuthus lamarmorai]]'' colonised Sardinia sometime after 450,000 years ago. It is suggested to have survived into the Last Glacial Period, until at least 60-30,000 years ago.<ref name=":14">{{Cite journal |last1=Palombo |first1=Maria Rita |last2=Zedda |first2=Marco |last3=Zoboli |first3=Daniel |date=March 2024 |title=The Sardinian Mammoth's Evolutionary History: Lights and Shadows |journal=Quaternary |language=en |volume=7 |issue=1 |pages=10 |doi=10.3390/quat7010010 |issn=2571-550X |doi-access=free}}</ref> |
The dwarf mammoth species ''[[Mammuthus lamarmorai]]'' descended from [[Steppe mammoth|steppe mammoths]] (''Mammuthus trogontherii'') that colonised Sardinia sometime after 450,000 years ago. It is suggested to have survived into the Last Glacial Period, until at least 60-30,000 years ago.<ref name=":14">{{Cite journal |last1=Palombo |first1=Maria Rita |last2=Zedda |first2=Marco |last3=Zoboli |first3=Daniel |date=March 2024 |title=The Sardinian Mammoth's Evolutionary History: Lights and Shadows |journal=Quaternary |language=en |volume=7 |issue=1 |pages=10 |doi=10.3390/quat7010010 |issn=2571-550X |doi-access=free}}</ref> |
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===Greece=== |
===Greece=== |
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⚫ | ''[[Mammuthus creticus]]'' is known from remains probably dating to the [[Early Pleistocene]]. It likely descends from ''[[Mammuthus meridionalis]]''. It is the smallest mammoth<ref name=":1">{{Cite journal |last1=Herridge |first1=V. L. |last2=Lister |first2=A. M. |year=2012 |title=Extreme insular dwarfism evolved in a mammoth |journal=Proceedings of the Royal Society B: Biological Sciences |volume=279 |issue=1741 |pages=3193–3300 |doi=10.1098/rspb.2012.0671 |pmc=3385739 |pmid=22572206}}</ref> and is among the smallest dwarf elephants known, with a shoulder height of about {{Convert|1|m|ft}} and a weight of about {{Convert|180|kg|lb}}.<ref name="proboscideans" /> ''[[Palaeoloxodon creutzburgi]]'' from the Middle Pleistocene and Late Pleistocene is significantly larger, with an estimated body mass comparable to living Asian elephant, around 40% the size of its mainland ancestor.<ref name=":0">{{Cite journal |last1=Athanassiou |first1=Athanassios |last2=van der Geer |first2=Alexandra A.E. |last3=Lyras |first3=George A. |date=August 2019 |title=Pleistocene insular Proboscidea of the Eastern Mediterranean: A review and update |url=https://linkinghub.elsevier.com/retrieve/pii/S0277379119300848 |journal=Quaternary Science Reviews |language=en |volume=218 |pages=306–321 |bibcode=2019QSRv..218..306A |doi=10.1016/j.quascirev.2019.06.028 |s2cid=199107354}}</ref><!-- http://rspb.royalsocietypublishing.org/content/early/2012/05/04/rspb.2012.0671 --> |
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Poulakakis and others proposed in 2002 to rename all the described specimens of larger size than ''Mammuthus creticus'' under the new subspecies name ''Elephas antiquus creutzburgi'' (Kuss, 1965).<ref>{{cite journal|author1=Poulakakis, N. |author2=Mylonas, M. |author3=Lymberakis, P. |author4=and Fassoulas, C. |date=2002-10-01| title = Origin and taxonomy of the fossil elephants of the island of Crete (Greece): problems and perspectives | journal = Palaeogeography, Palaeoclimatology, Palaeoecology | volume = 186 | issue = 1–2| pages = 163–183 | doi = 10.1016/S0031-0182(02)00451-0}}</ref> After DNA research, published in 2006, it has been proposed to rename ''Elephas (Palaeoloxodon) creticus'' into ''Mammuthus creticus'' (Bate, 1907). In a recent study of 2007, it was argued for the groundlessness of the theory by Poulakakis et al. in 2006,<ref name=Poulakakis2006>{{cite journal |author1=Poulakakis N. |author2=Parmakelis A. |author3=Lymberakis P. |author4=Mylonas M. |author5=Zouros E. |author6=Reese D. |author7=Glaberman S. |author8=Caccone A. | year = 2006 | title = Ancient DNA forces reconsideration of evolutionary history of Mediterranean pygmy elephantids | journal = Biol. Lett. | volume = 2 | issue = 3| pages = 451–454 | doi = 10.1098/rsbl.2006.0467 | pmid = 17148428 | pmc = 1686204 }}</ref> showing the weak points of that DNA research.<ref name="BioLetters">{{cite journal |author1=Orlando, L. |author2=Pagés, M. |author3=Calvignac, S. |display-authors=etal |date=2007-02-22 |title=Does the 43bp sequence from an 800000 year old Cretan dwarf elephantid really rewrite the textbook on mammoths? |journal=[[Biology Letters]] |volume=3 |issue=1 |pages=57–59 |doi=10.1098/rsbl.2006.0536 |pmc=2373798 |pmid=17443966}}</ref> However, morphological data is at least equivocal, and may also support placement in ''Mammuthus''. |
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⚫ | ''[[Mammuthus creticus]]'' is |
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====Cyclades==== |
====Cyclades==== |
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{{legend|lightgreen|connected during LGM<ref name="VanderGeer2014"/>}} |
{{legend|lightgreen|connected during LGM<ref name="VanderGeer2014"/>}} |
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Remains of dwarf elephants have been briefly reported from [[Paros]], [[Milos]] and [[Serifos]] in historical publications, but these lack any detailed information.<ref name=":0" /> |
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Remains of paleoloxodontine elephants have been reported from several Cyclades islands. The Delos elephant's size is comparable to ''Palaeoloxodon mnaidriensis''.<ref name="VanderGeer2014"/> The Naxos elephant has been described as ''Palaeoloxodon lomolinoi'' and it was smaller than the Delos elephant with a calculated body mass of only 10% of that of its mainland ancestor ''Palaeoloxodon antiquus''.<ref name="VanderGeer2014"/> |
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On [[Kythnos|Kýthnos]], the remains of a dwarf elephant were reported in a 1975 publication to be found associated with lithic artefacts. The age of the find was considered to be uncertain, likely older than 9,000 years, but could not be dated precisely due to a lack of collagen. Additionally, an isolated tusk was reported from the northwest of the island.<ref name=":0" /> |
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On [[Delos]], an indeterminate dwarf elephant known from a third molar was reported in 1908. This specimen clearly belongs to a dwarf species, but it is difficult to quantify its size precisely.<ref name=":0" /> On [[Naxos]] the species ''Palaeoloxodon lomolinoi'' has been described based on a partial skull including the maxilla bones and third molar teeth found near the Trypiti river, of probable Late Pleistocene age.''<ref name="VanderGeer2014" />'' It is estimated to be around 8% the size of ''P. antiquus'', and had a smaller body size than that represented by the dwarf elephant from Delos. The Eastern Cyclades islands of Delos, [[Naxos]], and Paros were connected during the [[Last Glacial Period]], which suggests that the Delos species and ''P. lomolinoi'' were not contemporaneous, with the former possibly being the ancestor of the latter, though nothing can be said for certain.<ref name=":0" /> |
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====Dodecanese==== |
====Dodecanese==== |
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| [[Astypalaia]] || ''Palaeoloxodon'' sp. || {{Smallcaps|Athanassiou}} et al., 2019<ref name="Athanassiou2019"/> |
| [[Astypalaia]] || ''Palaeoloxodon'' sp. || {{Smallcaps|Athanassiou}} et al., 2019<ref name="Athanassiou2019"/> |
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| [[Kasos]] || ''Palaeoloxodon'' [[Species affinis|aff.]] ''creutzburgi'' || {{Smallcaps|Sen}} et al., 2014<ref>{{cite journal | doi = 10.5735/086.051.0204| title = Late Pleistocene Dwarf Elephants from the Aegean Islands of Kassos and Dilos, Greece| journal = Annales Zoologici Fennici| volume = 51| pages = 27–42 | year = 2014| last1 = Sen | first1 = S.| last2 = Barrier | first2 = E.| last3 = Crété | first3 = X.| issue = 1–2| s2cid = 85190966}}</ref> |
| [[Kasos]] || ''Palaeoloxodon'' [[Species affinis|aff.]] ''creutzburgi'' || {{Smallcaps|Sen}} et al., 2014<ref name=":4">{{cite journal | doi = 10.5735/086.051.0204| title = Late Pleistocene Dwarf Elephants from the Aegean Islands of Kassos and Dilos, Greece| journal = Annales Zoologici Fennici| volume = 51| pages = 27–42 | year = 2014| last1 = Sen | first1 = S.| last2 = Barrier | first2 = E.| last3 = Crété | first3 = X.| issue = 1–2| s2cid = 85190966}}</ref> |
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| [[Rhodes]] || ''Palaeoloxodon'' sp. || {{Smallcaps|Symeonides}} et al., 1974 |
| [[Rhodes]] || ''Palaeoloxodon'' sp. || {{Smallcaps|Symeonides}} et al., 1974 |
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On [[Rhodes]], bones of an unnamed endemic dwarf elephant have been discovered in cave deposits on the east coast. This elephant was similar in size to ''Palaeoloxodon mnaidriensis,'' around 20% the size of its mainland ancestor. The remains, though temporally poorly constrained, are suggested to be Late Pleistocene age.<ref name=":0" /> Possible tracks produced by these dwarf elephants have been reported from the southwest of the island.<ref>{{Citation |last=Milàn |first=Jesper |title=A Diverse Vertebrate Ichnofauna from a Quaternary Eolian Oolite, Rhodes, Greece |date=2007 |work=Sediment–Organism InteractionsA Multifaceted Ichnology |url=https://pubs.geoscienceworld.org/books/book/1190/chapter/10726536 |access-date=2024-06-20 |publisher=SEPM Society for Sedimentary Geology |language=en |doi=10.2110/pec.07.88.0333 |isbn=978-1-56576-129-2 |last2=Bromley |first2=Richard G. |last3=Titschack |first3=Jürgen |last4=Theodorou |first4=Georgios}}</ref> |
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On the island of [[Rhodes]], bones of an endemic dwarf elephant have been discovered. This elephant was similar in size to ''Palaeoloxodon mnaidriensis''.<ref name=":0" /> |
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On [[Tilos]], the species ''Palaeoloxodon tiliensis'' has been described from remains found in Charkadio cave.<ref>G. Theodorou, N. Symeonidis, E. Stathopoulou ''Elephas tiliensis'' n. sp. from Tilos island (Dodecanese, Greece) Hell. J. Geosci., 42 (2007), pp. 19-32</ref> This species was medium-sized, around 10% the size of ''P. antiquus'', with a shoulder height of up to {{Convert|1.9|m|ft}}, with a body mass of {{Convert|630–890|kg|lb}}. Remains of the species are suggested to date to Late Pleistocene. Radiocarbon dating done in the 1970s suggested that the species survived until around 3,500 years ago, which would make the latest surviving ''Palaeoloxodon'' species and the youngest elephant in Europe, but these dates are tentative and await corroboration by other research.<ref name=":0" /> |
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Two groups of remains of dwarf elephants have been found on the island of [[Tilos]]. They are similar in size to ''Palaeoloxodon mnaidriensis'' and the smaller ''Palaeoloxodon falconeri'', but the two groups indicate sexual dimorphism.<ref name=Theodorou1983>{{cite book | author = Theodorou, G. | year = 1983 | title = The dwarf elephants of the Charkadio cave on the island of Tilos (Dodekanese, Greece) | publisher = Phd Thesis [[Athens University]] | page = 321 pp}}</ref><ref name=Theodorou1988>{{cite journal | author = Theodorou, G.E. | year = 1988 | title = Environmental factors affecting the evolution of islands endemics: The Tilos example for Greece | journal = Modern Geology | volume = 13 | pages = 183–188}}</ref> The remains had originally been designated to ''Palaeoloxodon antiquus falconeri'' (Busk, 1867). However, this name refers to the dwarf elephants from the island of Malta. As a result, since no migration route between the two islands can be proven, this name should not be used when referring to the elephant remnants from Tilos. The species has been described as ''Elephas tiliensis'' in 2007<ref name=Theodorou2007/> and it is now assigned to genus ''Palaeoloxodon''. |
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On [[Astypalaia]], a single tusk of a dwarf elephant of unknown age was excavated in the late 1990s. Due to the isolated status of the island it very likely represents an endemic species. Though the size of the animal is difficult to constrain precisely, it was probably similar in size to ''P. tiliensis''.<ref name=":0" /> |
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The Tilos dwarf elephant is the first dwarf elephant whose DNA sequence has been studied. The results of this research are consistent with previous morphological reports, according to which ''Palaeoloxodon'' is more closely related to ''Elephas'' than to ''Loxodonta'' or ''Mammuthus''.<ref>{{cite journal | last1=Poulakakis | first1=Nikos | last2=Theodorou | first2=Georgios E. | last3=Zouros | first3=Eleftherios | last4=Mylonas | first4=Moysis | title=Molecular Phylogeny of the Extinct Pleistocene Dwarf Elephant Palaeoloxodon antiquus falconeri from Tilos Island, Dodekanisa, Greece | journal=Journal of Molecular Evolution | publisher=Springer Science and Business Media LLC | volume=55 | issue=3 | date=2002-09-01 | issn=0022-2844 | doi=10.1007/s00239-002-2337-x | pages=364–374 | pmid=12187389| s2cid=21140948 }}</ref> On the other hand, DNA analysis in 2017 conclude that the closest living relative of the genus ''Palaeoloxodon'' is the [[African forest elephant]] (''Loxodonta cyclotis'').<ref name=Meyer>{{cite journal |last1=Meyer |first1=Matthias |last2=Palkopoulou |first2=Eleftheria |last3=Baleka |first3=Sina |last4=Stiller |first4=Mathias |last5=Penkman |first5=Kirsty E H |author5-link= Kirsty Penkman |last6=Alt |first6=Kurt W |last7=Ishida |first7=Yasuko |last8=Mania |first8=Dietrich |last9=Mallick |first9=Swapan |last10=Meijer |first10=Tom |last11=Meller |first11=Harald |last12=Nagel |first12=Sarah |last13=Nickel |first13=Birgit |last14=Ostritz |first14=Sven |last15=Rohland |first15=Nadin |last16=Schauer |first16=Karol |last17=Schüler |first17=Tim |last18=Roca |first18=Alfred L |last19=Reich |first19=David |last20=Shapiro |first20=Beth |last21=Hofreiter |first21=Michael |title=Palaeogenomes of Eurasian straight-tusked elephants challenge the current view of elephant evolution |journal=eLife |date=6 June 2017 |volume=6 |page=e25413 |doi=10.7554/eLife.25413 |pmid=28585920 |pmc=5461109 |doi-access=free}}</ref> The paper suggests that the current view of elephant evolution is "in need of substantial revision".<ref name=Meyer/> After the study of new osteological material<ref name=Theodorou2007/> that has been excavated in anatomical connection in the Charkadio Cave on Tilos island the new species name ''Palaeoloxodon tiliensis'' has been assigned to the Tilos dwarf elephants. |
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On [[Kasos]], which during the Pleistocene was connected with the islands of [[Karpathos]] and [[Saria Island|Saria]], a single dwarf ''Palaeoloxodon'' molar has been found. Due to the tooth closely resembling those of the species ''P. creutzburgi'' from Crete (which is adjacent to Kasos) in size and shape, it has been referred to as ''P.'' [[Species affinis|aff.]] ''creutzburgi.''<ref name=":4" /><ref name=":0" /> |
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===Cyprus=== |
===Cyprus=== |
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==The Channel Islands of California== |
==The Channel Islands of California== |
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[[File:M._exilis_skeletal.png|thumb|Skeletal restoration of ''Mammuthus exilis'']] |
[[File:M._exilis_skeletal.png|thumb|Skeletal restoration of ''Mammuthus exilis'']] |
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A population of the [[Mammoth|Columbian mammoth]] (''Mammuthus columbi'') arrived on the northern [[Channel Islands of California]] during the late Middle Pleistocene, around 250-150,000 years ago, giving rise to a dwarfed species, the [[pygmy mammoth]] (''Mammuthus exilis''). Channel Islands mammoths ranged from {{convert|150|–|190|cm|abbr=on}} in shoulder height. These mammoths became extinct around 13,000 years ago, around the time of arrival of modern humans to the islands.<ref name=":03">{{Cite journal |last1=Muhs |first1=Daniel R. |last2=Simmons |first2=Kathleen R. |last3=Groves |first3=Lindsey T. |last4=McGeehin |first4=John P. |last5=Randall Schumann |first5=R. |last6=Agenbroad |first6=Larry D. |date=May 2015 |title=Late Quaternary sea-level history and the antiquity of mammoths ( Mammuthus exilis and Mammuthus columbi ), Channel Islands National Park, California, USA |url=https://www.cambridge.org/core/product/identifier/S003358940000096X/type/journal_article |journal=Quaternary Research |language=en |volume=83 |issue=3 |pages=502–521 |bibcode=2015QuRes..83..502M |doi=10.1016/j.yqres.2015.03.001 |issn=0033-5894}}</ref><ref name=":15">{{Cite journal |last1=Semprebon |first1=Gina M. |last2=Rivals |first2=Florent |last3=Fahlke |first3=Julia M. |last4=Sanders |first4=William J. |last5=Lister |first5=Adrian M. |last6=Göhlich |first6=Ursula B. |date=June 2016 |title=Dietary reconstruction of pygmy mammoths from Santa Rosa Island of California |url=https://linkinghub.elsevier.com/retrieve/pii/S1040618215014020 |journal=Quaternary International |language=en |volume=406 |pages=123–136 |bibcode=2016QuInt.406..123S |doi=10.1016/j.quaint.2015.10.120}}</ref> |
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The [[Mammoth|Columbian mammoth]] (''Mammuthus columbi'') produced a separate, isolated population at the end of the Pleistocene on the [[Channel Islands of California]], most likely about 40,000 years ago (although the time of isolation is not fully known). Selective forces on the Channel Islands resulted in smaller animals, forming a new species, the [[pygmy mammoth]] (''Mammuthus exilis'').<ref>{{cite news |url=http://www.latimes.com/local/lanow/la-me-ln-mammoth-fossil-channel-islands-20160915-snap-story.html |title=Well-preserved mammoth skull unearthed on Channel Islands puzzles scientists |newspaper=[[Los Angeles Times]] |first=Veronica |last=Rocha |date=16 September 2016 |access-date=24 September 2016}}</ref> Channel Islands mammoths ranged from {{convert|150|–|190|cm|abbr=on}} in shoulder height. |
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⚫ | During the last ice age, [[woolly mammoth]]s (''Mammuthus primigenius'') lived on [[Wrangel Island]] in the [[Arctic Ocean]] and survived until 1700 BCE, the most recent survival of any known mammoth population. Wrangel Island is thought to have become separated from the mainland by 12000 BCE. It was assumed that Wrangel Island mammoths ranged from {{convert|180|–|230|cm|abbr=on}} in shoulder height and were for a time considered "dwarf mammoths".<ref name=Nature>{{cite journal |author1=Vartanyan, S.L. |author2=Garutt, V.E. |author3=Sher, A.V. | |
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==Indonesia and the Philippines== |
==Indonesia and the Philippines== |
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=== Mindanao === |
=== Mindanao === |
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On the island of [[Mindanao]], the dwarf ''Stegodon'' species ''Stegodon mindanensis'' was present at some point in the Pleistocene. It has an estimated body mass of around {{Convert|400|kg|lb}}.<ref>{{Cite book |last=Ong |first=Perry |url=https://www.researchgate.net/publication/303496589 |title=The Philippine Archipelago |publisher=Asia Publishing Co. Ltd. |year=1998 |location=Makati city, Philippines |pages=227–255 |chapter=The Philippine Menagerie}}</ref> |
On the island of [[Mindanao]], the dwarf ''Stegodon'' species ''Stegodon mindanensis'' was present at some point in the Pleistocene. It has an estimated body mass of around {{Convert|400|kg|lb}}.<ref>{{Cite book |last=Ong |first=Perry |url=https://www.researchgate.net/publication/303496589 |title=The Philippine Archipelago |publisher=Asia Publishing Co. Ltd. |year=1998 |location=Makati city, Philippines |pages=227–255 |chapter=The Philippine Menagerie}}</ref> |
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== Japan == |
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Some species of the stegodontid ''[[Stegolophodon]]'' from the Middle [[Miocene]] of Japan around 16 million years ago have been suggested to exhibit insular dwarfism, which would make them the oldest known proboscideans to do so.<ref>{{Cite journal |last=Saegusa |first=Haruo |date=May 2008 |title=Dwarf Stegolophodon from the Miocene of Japan: Passengers on sinking boats |url=https://linkinghub.elsevier.com/retrieve/pii/S1040618207002273 |journal=Quaternary International |language=en |volume=182 |issue=1 |pages=49–62 |doi=10.1016/j.quaint.2007.08.001}}</ref><ref>{{Cite journal |last=Hunt |first=David A. G. A. |last2=DiBattista |first2=Joseph D. |last3=Hendry |first3=Andrew P. |date=May 2022 |title=Effects of insularity on genetic diversity within and among natural populations |url=https://onlinelibrary.wiley.com/doi/10.1002/ece3.8887 |journal=Ecology and Evolution |language=en |volume=12 |issue=5 |doi=10.1002/ece3.8887 |issn=2045-7758|hdl=10072/425158 |hdl-access=free }}</ref> |
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During Pliocene-Early Pleistocene (from around 4-1 million years ago), a succession of endemic dwarf species of ''Stegodon,'' probably representing a single lineage lived in the [[Japanese archipelago]], probably derived from the mainland Chinese ''S. zydanskyi.'' In chronological succession these species are ''Stegodon miensis'' (4-3 million years ago) ''Stegodon protoaurorae'' (3-2 million years ago) and ''[[Stegodon aurorae]],'' (2-1 million years ago) which show a progressive size reduction through time, possibly as a result of reducing land area of the Japanese archipelago.<ref>{{Cite journal |last=Aiba |first=Hiroaki |last2=Baba |first2=Katsuyoshi |last3=Matsukawa |first3=Masaki |date=2010-03-10 |title=A new species of Stegodon (Mammalia, Proboscidea) from the Kazusa Group (lower Pleistocene), Hachioji City, Tokyo, Japan and its evolutionary morphodynamics: STEGODON PROTOAURORAE SP. NOV. AND MORPHODYNAMICS |url=https://onlinelibrary.wiley.com/doi/10.1111/j.1475-4983.2010.00953.x |journal=Palaeontology |language=en |volume=53 |issue=3 |pages=471–490 |doi=10.1111/j.1475-4983.2010.00953.x}}</ref> The latest and smallest species ''S. aurorae'' is estimated to be 25% the size of its mainland ancestor with a body mass of around {{Convert|2122|kg|lb}}.<ref name="Geer-2016" /> |
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⚫ | |||
⚫ | During the last ice age, [[woolly mammoth]]s (''Mammuthus primigenius'') lived on [[Wrangel Island]] in the [[Arctic Ocean]] and survived until 1700 BCE, the most recent survival of any known mammoth population. Wrangel Island is thought to have become separated from the mainland by 12000 BCE. It was assumed that Wrangel Island mammoths ranged from {{convert|180|–|230|cm|abbr=on}} in shoulder height and were for a time considered "dwarf mammoths".<ref name="Nature">{{cite journal |author1=Vartanyan, S.L. |author2=Garutt, V.E. |author3=Sher, A.V. |year=1993 |title=Holocene dwarf mammoths from Wrangel Island in the Siberian Arctic |journal=[[Nature (journal)|Nature]] |volume=362 |issue=6418 |pages=337–340 |doi=10.1038/362337a0 |pmid=29633990 |s2cid=4249191}}</ref> However this classification has been re-evaluated and since the Second International Mammoth Conference in 1999, these mammoths are no longer considered to be true "dwarf mammoths".<ref>{{cite journal |last=Tikhonov |first=Alexei |author2=Larry Agenbroad |author3=Sergey Vartanyan |year=2003 |title=Comparative analysis of the mammoth populations on Wrangel Island and the Channel Islands |url=http://www.nmr.nl/nmr/pages/showPage.do?itemid=1896&instanceid=16 |url-status=dead |journal=Deinsea |volume=9 |pages=415–420 |issn=0923-9308 |archive-url=https://web.archive.org/web/20120611113051/http://www.nmr.nl/nmr/pages/showPage.do?itemid=1896&instanceid=16 |archive-date=2012-06-11}}</ref> |
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==See also== |
==See also== |
Revision as of 20:57, 14 July 2024
Dwarf elephants are prehistoric members of the order Proboscidea which, through the process of allopatric speciation on islands, evolved much smaller body sizes (around 1–2.3 metres (3 ft 3 in – 7 ft 7 in) shoulder height) in comparison with their immediate ancestors. Dwarf elephants are an example of insular dwarfism, the phenomenon whereby large terrestrial vertebrates (usually mammals) that colonize islands evolve dwarf forms, a phenomenon attributed to adaptation to resource-poor environments and lack of predation and competition.
Fossil remains of dwarf elephants have been found on the Mediterranean islands of Cyprus, Malta, Crete, Sicily, Sardinia, the Cyclades Islands and the Dodecanese Islands, which are mostly members of the genus Palaeoloxodon, descending from the large 4 metres (13 ft) tall mainland European species Palaeoloxodon antiquus, though two species represent dwarf mammoths. Dwarf species of elephants and Stegodon have been found on the islands of Indonesia and the Philippines, with dwarfed species of Stegodon also having been found in Japan. The Channel Islands of California once supported a dwarf species descended from Columbian mammoths,[1] while the woolly mammoths that existed on Wrangel Island north of Siberia were once considered dwarfs, but are not anymore.
The Mediterranean islands
Dwarf elephants first inhabited the Mediterranean islands during the Pleistocene, including all the major islands with the apparent exception of Corsica and the Balearics. Mediterranean dwarf elephants have generally been considered as members of the genus Palaeoloxodon, derived from the continental straight-tusked elephant, Palaeoloxodon antiquus (Falconer & Cautley, 1847), Syn.: Elephas antiquus. An exception is the dwarf Middle-Late Pleistocene Sardinian mammoth, Mammuthus lamarmorai (Major, 1883), the first endemic elephant of the Mediterranean islands recognized as belonging to the mammoth line. Mammuthus creticus from the Early Pleistocene of Crete, formerly considered a member of Palaeoloxodon, is now also considered to be a mammoth, and approaches the size of the smallest dwarf elephants.[3]
During low sea levels, the Mediterranean islands were colonised again and again, giving rise, sometimes on the same island, to several species (or subspecies) of different body sizes. As the Ice Age came to an end, sea levels rose, stranding elephants on the island. The island of Sicily appears to have been colonised by proboscideans in at least three separate waves of colonisation. These endemic dwarf elephants were taxonomically different on each island or group of very close islands, like the Cyclades archipelago.
There are many uncertainties about the time of colonisation, the phylogenetic relationships and the taxonomic status of dwarf elephants on the Mediterranean islands. Extinction of the insular dwarf elephants has not been correlated with the arrival of humans to the islands. Furthermore, it has been suggested by the palaeontologist Othenio Abel in 1914,[4] that the finding of skeletons of such elephants sparked the idea that they belonged to giant one-eyed monsters, because the center nasal opening was thought to be the socket of a single eye, and thus perhaps were, for example, the origin of the one-eyed Cyclopes of Greek mythology.
Italy and Malta
Island | Taxon | Author |
---|---|---|
Sardinia | Mammuthus lamarmorai | (Major, 1883) |
Malta | Palaeoloxodon falconeri | (Busk, 1869) |
Palaeoloxodon mnaidriensis | (Adams, 1874) | |
Sicily | Palaeoloxodon falconeri | (Busk, 1869) |
Palaeoloxodon cf. mnaidriensis | (Adams, 1874) |
Sicily and Malta were inhabited by two successive waves of dwarf elephants derived from P. antiquus, which first arrived on the islands at least 500,000 years ago. The first of these species is P. falconeri , which is one of the smallest dwarf elephant species at around 1 metre (3.3 ft) tall, and was strongly modified from its ancestor in numerous aspects, which lived in a depauperate fauna with no other large mammal species.[6][7] Later, around 200,000 years ago, this species was replaced by a second colonisation by P. antiquus, which gave rise to the larger (though still considerably dwarfed) 2 metres (6.6 ft) tall species P. mnaidriensis, which on Sicily lived alongside a number other large mammal species, including herbivores and carnivores.[7][8][9] The youngest records of this species on Sicily date to around 20,000 years ago, close to the time of arrival of modern humans on Sicily.[10]
The dwarf mammoth species Mammuthus lamarmorai descended from steppe mammoths (Mammuthus trogontherii) that colonised Sardinia sometime after 450,000 years ago. It is suggested to have survived into the Last Glacial Period, until at least 60-30,000 years ago.[11]
Greece
Crete
Island | Taxon | Author |
---|---|---|
Crete | Mammuthus creticus | (Bate, 1907) |
Palaeoloxodon creutzburgi | (Kuss, 1965) |
Mammuthus creticus is known from remains probably dating to the Early Pleistocene. It likely descends from Mammuthus meridionalis. It is the smallest mammoth[12] and is among the smallest dwarf elephants known, with a shoulder height of about 1 metre (3.3 ft) and a weight of about 180 kilograms (400 lb).[13] Palaeoloxodon creutzburgi from the Middle Pleistocene and Late Pleistocene is significantly larger, with an estimated body mass comparable to living Asian elephant, around 40% the size of its mainland ancestor.[14]
Cyclades
Island | Taxon | Author |
---|---|---|
Delos | Palaeoloxodon sp. | Vaufrey, 1929 |
Naxos | Palaeoloxodon lomolinoi | Van der Geer et al., 2014[15] |
Paros | Elephantidae indet. | Georgalas, 1929 |
Kythnos | Elephantidae indet. | Honea, 1975 |
Milos | Elephantidae indet. | Papp, 1953 |
Serifos | Elephantidae indet. | Papp, 1953 |
Remains of dwarf elephants have been briefly reported from Paros, Milos and Serifos in historical publications, but these lack any detailed information.[14]
On Kýthnos, the remains of a dwarf elephant were reported in a 1975 publication to be found associated with lithic artefacts. The age of the find was considered to be uncertain, likely older than 9,000 years, but could not be dated precisely due to a lack of collagen. Additionally, an isolated tusk was reported from the northwest of the island.[14]
On Delos, an indeterminate dwarf elephant known from a third molar was reported in 1908. This specimen clearly belongs to a dwarf species, but it is difficult to quantify its size precisely.[14] On Naxos the species Palaeoloxodon lomolinoi has been described based on a partial skull including the maxilla bones and third molar teeth found near the Trypiti river, of probable Late Pleistocene age.[15] It is estimated to be around 8% the size of P. antiquus, and had a smaller body size than that represented by the dwarf elephant from Delos. The Eastern Cyclades islands of Delos, Naxos, and Paros were connected during the Last Glacial Period, which suggests that the Delos species and P. lomolinoi were not contemporaneous, with the former possibly being the ancestor of the latter, though nothing can be said for certain.[14]
Dodecanese
Island | Taxon | Author |
---|---|---|
Astypalaia | Palaeoloxodon sp. | Athanassiou et al., 2019[2] |
Kasos | Palaeoloxodon aff. creutzburgi | Sen et al., 2014[16] |
Rhodes | Palaeoloxodon sp. | Symeonides et al., 1974 |
Tilos | Palaeoloxodon tiliensis | (Theodorou et al. 2007)[17] |
On Rhodes, bones of an unnamed endemic dwarf elephant have been discovered in cave deposits on the east coast. This elephant was similar in size to Palaeoloxodon mnaidriensis, around 20% the size of its mainland ancestor. The remains, though temporally poorly constrained, are suggested to be Late Pleistocene age.[14] Possible tracks produced by these dwarf elephants have been reported from the southwest of the island.[18]
On Tilos, the species Palaeoloxodon tiliensis has been described from remains found in Charkadio cave.[19] This species was medium-sized, around 10% the size of P. antiquus, with a shoulder height of up to 1.9 metres (6.2 ft), with a body mass of 630–890 kilograms (1,390–1,960 lb). Remains of the species are suggested to date to Late Pleistocene. Radiocarbon dating done in the 1970s suggested that the species survived until around 3,500 years ago, which would make the latest surviving Palaeoloxodon species and the youngest elephant in Europe, but these dates are tentative and await corroboration by other research.[14]
On Astypalaia, a single tusk of a dwarf elephant of unknown age was excavated in the late 1990s. Due to the isolated status of the island it very likely represents an endemic species. Though the size of the animal is difficult to constrain precisely, it was probably similar in size to P. tiliensis.[14]
On Kasos, which during the Pleistocene was connected with the islands of Karpathos and Saria, a single dwarf Palaeoloxodon molar has been found. Due to the tooth closely resembling those of the species P. creutzburgi from Crete (which is adjacent to Kasos) in size and shape, it has been referred to as P. aff. creutzburgi.[16][14]
Cyprus
Island | Taxon | Author |
---|---|---|
Cyprus | Palaeoloxodon cypriotes | (Bate, 1903)[20] |
Palaeoloxodon xylophagou | Athanassiou et al., 2015[21] |
The Cyprus dwarf elephant (Palaeoloxodon cypriotes) survived at least until 12,000 years ago, around the time of arrival of modern humans to Cyprus (who may have hunted it), making it one of the latest surviving dwarf elephants. It is also one of the smallest dwarf elephant species, comparable in size to P. falconeri, with an estimated shoulder height of 1 metre (3.3 ft). The species likely evolved from the earlier larger (though still strongly dwarfed) Palaeoloxodon xylophagou known from fossils dating to around 200,000 years ago.[22]
Remains of the species were first discovered and recorded by Dorothea Bate in a cave in the Kyrenia hills of northern Cyprus in 1902 and reported in 1903.[20][23]
The Channel Islands of California
A population of the Columbian mammoth (Mammuthus columbi) arrived on the northern Channel Islands of California during the late Middle Pleistocene, around 250-150,000 years ago, giving rise to a dwarfed species, the pygmy mammoth (Mammuthus exilis). Channel Islands mammoths ranged from 150–190 cm (59–75 in) in shoulder height. These mammoths became extinct around 13,000 years ago, around the time of arrival of modern humans to the islands.[24][25]
Indonesia and the Philippines
In Indonesia and the Philippines, evidence of a succession of distinct endemic island faunas has been found, including dwarfed elephants and species of Stegodon.
Flores
During the late Early Pleistocene, Flores was inhabited by the dwarf species Stegodon sondaarii, around 15% of the size of mainland Stegodon species, which was around 120 cm (3.9 ft) tall at the shoulder and weighed about 350–400 kilograms (770–880 lb). This species became extinct around 1 million years ago,[13][26][27] being replaced by Stegodon florensis. Stegodon florensis shows a progressive size reduction with time, with the earlier Middle Pleistocene subspecies Stegodon florensis florensis estimated to be around 50% the size of mainland Stegodon species with a shoulder height of around 190 cm (6.2 ft) and a body mass of around 1.7 tons, while the later Stegodon florensis insularis from the Late Pleistocene is estimated to be around 17% the size of mainland Stegodon species, with a shoulder height of around 130 cm (4.3 ft), and a body mass of about 570 kilograms (1,260 lb) [27][28] Stegodon florensis became extinct about 50,000 years ago, around the time of the arrival of modern humans to Flores.[26]
Sulawesi
During the Late Pliocene-Early Pleistocene on Sulawesi, two species of dwarf proboscidean coinhabited the island, the elephant Stegoloxodon celebensis, and Stegodon sompoensis.[29] The former was about 150 cm (4.9 ft) tall,[30] while the latter was around 32% the size of mainland Stegodon species, with an estimated body mass of about a ton.[27] Later in the Pleistocene, these animals were replaced by larger-sized species of Stegodon and elephants,[29][31] with an indeterminate Stegodon species from the Middle Pleistocene of Sulawesi being around 57% the size of mainland species, with an estimated bodymass of about 2 tons.[27]
Java
The species Stegodon trigonocephalus is known from the Early-Middle Pleistocene of Java.[32] A population from the Trinil H.K locality, which likely dates to the Middle Pleistocene,[33] is around 65% the size of mainland Stegodon species.[27] Large individuals are estimated to have reached around 280 cm (9.2 ft) at the shoulders, with a body mass of around 5 tons.[13] Other smaller unnamed Stegodon species are also known from the Early Pleistocene on the island.[32] The extinct dwarf elephant species Stegoloxodon indonesicus is also known from the Early Pleistocene of Java, which is probably closely related to S. celebensis from Sulawesi, but whose relationships to other elephants are obscure.[34][32]
Sumba
The species Stegodon sumbaensis of an uncertain Middle-Late Pleistocene age from Sumba is one the smallest known species, at around 8% of the size of its mainland ancestor, with an estimated body mass of around 250 kilograms (550 lb).[27]
Timor
The species Stegodon timorensis is known from the Middle Pleistocene of Timor. It is a small-sized species, only slightly larger than S. sondaarii,[35] and around 23% the size of mainland species, with an estimated body mass of around 770 kilograms (1,700 lb).[27]
Luzon
On Luzon the dwarf Stegodon luzonensis is known from remains found in the Manila Basin of an uncertain Pleistocene age,[36] as well as remains found near the early Middle Pleistocene Nesorhinus butchery site.[37] It is around 40% the size of mainland Stegodon species, with a body mass of around 1.3 tons.[27] The extinct dwarf elephant Elephas beyeri is also known from the island,[27] which is estimated to have been about 1.2 metres (3.9 ft) in shoulder height.[38]
Mindanao
On the island of Mindanao, the dwarf Stegodon species Stegodon mindanensis was present at some point in the Pleistocene. It has an estimated body mass of around 400 kilograms (880 lb).[39]
Japan
Some species of the stegodontid Stegolophodon from the Middle Miocene of Japan around 16 million years ago have been suggested to exhibit insular dwarfism, which would make them the oldest known proboscideans to do so.[40][41]
During Pliocene-Early Pleistocene (from around 4-1 million years ago), a succession of endemic dwarf species of Stegodon, probably representing a single lineage lived in the Japanese archipelago, probably derived from the mainland Chinese S. zydanskyi. In chronological succession these species are Stegodon miensis (4-3 million years ago) Stegodon protoaurorae (3-2 million years ago) and Stegodon aurorae, (2-1 million years ago) which show a progressive size reduction through time, possibly as a result of reducing land area of the Japanese archipelago.[42] The latest and smallest species S. aurorae is estimated to be 25% the size of its mainland ancestor with a body mass of around 2,122 kilograms (4,678 lb).[27]
Wrangel Island
During the last ice age, woolly mammoths (Mammuthus primigenius) lived on Wrangel Island in the Arctic Ocean and survived until 1700 BCE, the most recent survival of any known mammoth population. Wrangel Island is thought to have become separated from the mainland by 12000 BCE. It was assumed that Wrangel Island mammoths ranged from 180–230 cm (71–91 in) in shoulder height and were for a time considered "dwarf mammoths".[43] However this classification has been re-evaluated and since the Second International Mammoth Conference in 1999, these mammoths are no longer considered to be true "dwarf mammoths".[44]
See also
References
- ^ "The Pygmy Mammoth (U.S. National Park Service)".
- ^ a b Athanassiou, A.; Van der Geer, A. A. E.; Lyras, G. A. (2019). "Pleistocene insular Proboscidea of the Eastern Mediterranean: A review and update". Quaternary Science Reviews. 218: 306–321. Bibcode:2019QSRv..218..306A. doi:10.1016/j.quascirev.2019.06.028. S2CID 199107354.
- ^ Herridge, Victoria L.; Lister, Adrian M. (2012-05-09). "Extreme insular dwarfism evolved in a mammoth". Proceedings of the Royal Society B: Biological Sciences. 279 (1741): 3193–3200. doi:10.1098/rspb.2012.0671. ISSN 0962-8452. PMC 3385739. PMID 22572206.
- ^ Abel's surmise is noted by Adrienne Mayor in The First Fossil Hunters: Paleontology in Greek and Roman Times (Princeton University Press) 2000. [See illus. ed., 2001: ISBN 0691089779]
- ^ Palombo, M. R.; Antonioli, F.; Di Patti, C.; Presti, V. L.; Scarborough, M. E. (2020). "Was the dwarfed Palaeoloxodon from Favignana Island the last endemic Pleistocene elephant from the western Mediterranean islands?". Historical Biology. 33 (10): 1–19. doi:10.1080/08912963.2020.1772251. S2CID 225710152.
- ^ Bonfiglio, L., Marra, A. C., Masini, F., Pavia, M., & Petruso, D. (2002). Pleistocene faunas of Sicily: a review. In W. H. Waldren, & J. A. Ensenyat (Eds.), World islands in prehistory: international insular investigations. British Archaeological Reports, International Series, 1095, 428–436.
- ^ a b Scarborough, Matthew Edward (March 2022). "Extreme Body Size Variation in Pleistocene Dwarf Elephants from the Siculo-Maltese Palaeoarchipelago: Disentangling the Causes in Time and Space". Quaternary. 5 (1): 17. doi:10.3390/quat5010017. hdl:11427/36354. ISSN 2571-550X.
- ^ Baleka, Sina; Herridge, Victoria L.; Catalano, Giulio; Lister, Adrian M.; Dickinson, Marc R.; Di Patti, Carolina; Barlow, Axel; Penkman, Kirsty E.H.; Hofreiter, Michael; Paijmans, Johanna L.A. (August 2021). "Estimating the dwarfing rate of an extinct Sicilian elephant". Current Biology. 31 (16): 3606–3612.e7. doi:10.1016/j.cub.2021.05.037. PMID 34146486. S2CID 235477150.
- ^ Bethune, Elehna; Kaiser, Thomas M.; Schulz-Kornas, Ellen; Winkler, Daniela E. (November 2019). "Multiproxy dietary trait reconstruction in Pleistocene Hippopotamidae from the Mediterranean islands". Palaeogeography, Palaeoclimatology, Palaeoecology. 533: 109210. Bibcode:2019PPP...533j9210B. doi:10.1016/j.palaeo.2019.05.032. S2CID 181824675.
- ^ Palombo, Maria Rita; Antonioli, Fabrizio; Di Patti, Carolina; Valeria, Lo Presti; Scarborough, Matthew E. (2021-10-03). "Was the dwarfed Palaeoloxodon from Favignana Island the last endemic Pleistocene elephant from the western Mediterranean islands?". Historical Biology. 33 (10): 2116–2134. doi:10.1080/08912963.2020.1772251. ISSN 0891-2963. S2CID 225710152.
- ^ Palombo, Maria Rita; Zedda, Marco; Zoboli, Daniel (March 2024). "The Sardinian Mammoth's Evolutionary History: Lights and Shadows". Quaternary. 7 (1): 10. doi:10.3390/quat7010010. ISSN 2571-550X.
- ^ Herridge, V. L.; Lister, A. M. (2012). "Extreme insular dwarfism evolved in a mammoth". Proceedings of the Royal Society B: Biological Sciences. 279 (1741): 3193–3300. doi:10.1098/rspb.2012.0671. PMC 3385739. PMID 22572206.
- ^ a b c Larramendi, A. (2016). "Shoulder height, body mass and shape of proboscideans" (PDF). Acta Palaeontologica Polonica. 61. doi:10.4202/app.00136.2014. S2CID 2092950.
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