“Glacial refugium”的意思、由来-开放百科全书

A glacial refugium (plural refugia) is a geographic region which made possible the survival of flora and fauna in times of ice ages and allowed for post-glacial re-colonization.^[1] Different types of glacial refugia can be distinguished, namely nunatak, peripheral and lowland refugia.^[2] Glacial refugia have been suggested as a major cause of the distributions of flora and fauna in both temperate and tropical latitudes.^[3]^[4]^[5] However, in spite of the continuing use of historical refugia to explain modern-day species distributions, especially in birds,^[6]^[7] doubt has been cast on the validity of such inferences, as much of the differentiation between populations observed today may have occurred before or after their restriction to refugia.^[8]^[9]

Identification of Glacial Refugia

Traditionally, the identification of glacial refugia have occurred through the assessment of palaeoecological evidence, to determine the origins of modern taxa.^[4] For example, paleoecological approaches, which focus on the study of fossil organisms and their remains, have been used to reconstruct the distributions of pollen in Europe, for the 13,000 years since the last glaciation. Researchers in this case ultimately established the spread of forest trees from the mountainous southern fringe of Europe, which suggests that this area served as a glacial refugia during this time.^[10]

Different Types of Glacial Refugia

In studies exploring the extent of glacial refugia in mountain species, three distinct types of glacial refugia have been identified.^[2]

Nunatak Glacial Refugia

A nunatak is a type of glacial refugia that is located on the snow-free, exposed peaks of mountains, which lie above the ice sheet during glaciations.^[2] The identification of ‘diversity hotspots’ in areas, which should have been migration regions during major glacial episodes, is evidence for nunatak glacial refugia.^[11] For example, the Monte Rosa mountain ranges, the Avers, and the Engadine and the Bernina are all floristically rich proposed nunatak regions, which are indicative nunatak glacial survival.^[11]

Peripheral Glacial Refugia

Peripheral glacial refugia still exists within the mountain system but contrary to nunataks, which exist on the peaks, this type of refugia is located along the borders of mountain systems.^[2] Evidence for this type of mountain refugia can be found along the borders of the Carpathian Mountains, Pyrenees or European Alps, all of which were formally glaciated mountain systems. Specifically, using the amplified fragment length polymorphism (AFLP) technique, researchers have been able to infer the survival of Phyteuma globulariifolium in peripheral refugia, in the European Alps.^[12]

Lowland Glacial Refugia

Lowland glacial refugia, unlike nunatak and peripheral glacial refugia, is a type of refugia that exists outside of the mountain system in the lowlands.^[2] Situated beyond the limits of ice shields, lowland refugia has been identified for a number of plant and animal species. For example, through allozyme analysis, researchers have been able to confirm the continuous distribution of Zygaena exulans in the between the foothills of the Pyrenees and the Alps during the last ice age.^[13]

See also

References

1. ^The encyclopedia of earth, http://www.eoearth.org/view/article/155685/
2. ^¹²³⁴Holderegger, R., Thiel-Egenter, C. (2009): A discussion of different types of glacial refugia used in mountain biogeography and phytogeography. Journal of Biogeography 36, 476-480.
3. ^{{Cite journal|last=Petit|first=Rémy J.|last2=Aguinagalde|first2=Itziar|last3=Beaulieu|first3=Jacques-Louis de|last4=Bittkau|first4=Christiane|last5=Brewer|first5=Simon|last6=Cheddadi|first6=Rachid|last7=Ennos|first7=Richard|last8=Fineschi|first8=Silvia|last9=Grivet|first9=Delphine|date=2003-06-06|title=Glacial Refugia: Hotspots But Not Melting Pots of Genetic Diversity|url=http://science.sciencemag.org/content/300/5625/1563|journal=Science|volume=300|issue=5625|pages=1563–1565|doi=10.1126/science.1083264|issn=0036-8075|pmid=12791991}}
4. ^¹{{Cite journal|last=PROVAN|first=J|last2=BENNETT|first2=K|date=2008-10-01|title=Phylogeographic insights into cryptic glacial refugia|url=http://www.cell.com/trends/ecology-evolution/fulltext/S0169-5347(08)00249-8?_returnURL=http://linkinghub.elsevier.com/retrieve/pii/S0169534708002498?showall=true|journal=Trends in Ecology & Evolution|language=English|volume=23|issue=10|pages=564–571|doi=10.1016/j.tree.2008.06.010|issn=0169-5347}}
5. ^{{Cite journal|last=Rull|first=Valentí|date=2011-10-01|title=Neotropical biodiversity: timing and potential drivers|url=http://www.cell.com/trends/ecology-evolution/abstract/S0169-5347(11)00144-3|journal=Trends in Ecology & Evolution|language=English|volume=26|issue=10|pages=508–513|doi=10.1016/j.tree.2011.05.011|issn=0169-5347|pmid=21703715}}
6. ^{{Cite journal|last=Brumfield|first=Robb T.|date=2012-07-01|title=Inferring the Origins of Lowland Neotropical Birds|url=http://www.bioone.org/doi/abs/10.1525/auk.2012.129.3.367|journal=The Auk|volume=129|issue=3|pages=367–376|doi=10.1525/auk.2012.129.3.367|issn=0004-8038}}
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8. ^{{Cite journal|last=Klicka|first=John|last2=Zink|first2=Robert M.|date=1997-09-12|title=The Importance of Recent Ice Ages in Speciation: A Failed Paradigm|url=http://science.sciencemag.org/content/277/5332/1666|journal=Science|volume=277|issue=5332|pages=1666–1669|doi=10.1126/science.277.5332.1666|issn=0036-8075}}
9. ^{{Cite journal|last=Colinvaux|first=P. A.|last2=De Oliveira|first2=P. E.|last3=Bush|first3=M. B.|date=2000-01-01|title=Amazonian and neotropical plant communities on glacial time-scales: The failure of the aridity and refuge hypotheses|url=http://www.sciencedirect.com/science/article/pii/S0277379199000591|journal=Quaternary Science Reviews|volume=19|issue=1–5|pages=141–169|doi=10.1016/S0277-3791(99)00059-1}}
10. ^{{Cite journal|last=Munaut|first=André-V.|date=May 1986|title=An Atlas of past and present pollen maps of Europe: 0–13,000 years ago|url=http://dx.doi.org/10.1016/0034-6667(86)90044-8|journal=Review of Palaeobotany and Palynology|volume=47|issue=3-4|pages=411–412|doi=10.1016/0034-6667(86)90044-8|issn=0034-6667}}
11. ^¹{{Cite book|title=Nunataks and peripheral refugia for alpine plants during quaternary glaciation in the middle part of the Alps|last=Stehlik, Ivana|date=2000-06-01|publisher=Birkhäuser|oclc=753524599}}
12. ^{{Cite journal|last=Schönswetter|first=P.|last2=Tribsch|first2=A.|last3=Barfuss|first3=M.|last4=Niklfeld|first4=H.|date=December 2002|title=Several Pleistocene refugia detected in the high alpine plant Phyteuma globulariifolium Sternb. & Hoppe (Campanulaceae) in the European Alps|url=http://dx.doi.org/10.1046/j.1365-294x.2002.01651.x|journal=Molecular Ecology|volume=11|issue=12|pages=2637–2647|doi=10.1046/j.1365-294x.2002.01651.x|issn=0962-1083}}
13. ^{{Cite journal|last=Schmitt|first=Thomas|last2=Hewitt|first2=Godfrey M.|date=2004-05-07|title=Molecular biogeography of the arctic-alpine disjunct burnet moth species Zygaena exulans (Zygaenidae, Lepidoptera) in the Pyrenees and Alps|url=http://dx.doi.org/10.1111/j.1365-2699.2004.01079.x|journal=Journal of Biogeography|volume=31|issue=6|pages=885–893|doi=10.1111/j.1365-2699.2004.01079.x|issn=0305-0270}}