Share to: share facebook share twitter share wa share telegram print page

Glacial relict

A photo of a flowering shrub - the photo centers on a single white flower at the end of a branch with red leaves (as the photo was taken in the autumn).
The Franklin tree is an example of a glacial relict species from the Southeastern USA. It went extinct in the wild in the early 19th century due to a changing climate, inability to spread outside of its limited range, and limited environmental tolerance. The species survives today as a cultivated garden plant.

A glacial relict is a population of a species previously common during a glacial period that retreated into refugia during interglacial periods.[1] They are typically cold-adapted species with a distribution restricted to regions and microhabitats that allow them to survive despite climatic changes.[1][2]

Examples

There are a wide variety of plant species which fit the category of glacial relict. The ones given here are a small selection of the much larger group.

  • The biogeography of various aquatic species deemed glacial relicts that are found in Lake Sommen is likely related to a different geography during the early history of the lake. One theory claims that aquatic species were transferred from the Baltic Ice Lake through a natural lock system in connection with a temporary advance of the ice-front during the Younger Dryas.[3] On land, the unusual occurrence of dwarf birch near Sund is also judged to be a leftover from a cold geological past.[4]
  • The Franklin tree (Franklinia alatamaha) was a glacial relict in the American Southeast and endemic to the Altamaha River valley in Georgia before going extinct in the wild in the early part of the 19th century.[5] Like various other plants in this region of the United States, it grew in a lowland glacial refuge. Due to changing temperatures in the Holocene, it was unable to survive - it likely originally dispersed as seeds floating down the Altamaha River, but due to the nature of rivers, it was unable to make the reverse journey to cooler upland climes and survive rising temperatures.[6] This species was the subject of a number of enthusiastic searches to locate potential wild populations in the 20th century, but it was never found in the wild after its original extinction[5] and reintroduction efforts in the early 21st century failed.[6]

See also

References

  1. ^ a b Dítě, Daniel; Hájek, Michal; Svitková, Ivana; Košuthová, Alica; Šoltés, Rudolf; Kliment, Ján (September 2018). "Glacial-relict symptoms in the Western Carpathian flora". Folia Geobotanica. 53 (3): 277–300. doi:10.1007/s12224-018-9321-8.
  2. ^ Jiménez-Alfaro, Borja; García-Calvo, Laura; García, Pedro; Acebes, José Luis (2016). "Anticipating extinctions of glacial relict populations in mountain refugia". Biological Conservation. 201: 243–251. doi:10.1016/j.biocon.2016.07.015.
  3. ^ Kinsten, Björn (2010). De glacialrelikta kräftdjurens utbredning i södra Sverige (Götaland och Svealand) (PDF) (Report) (in Swedish). Länsstyrelsen Blekinge län. pp. 1–19. Retrieved April 19, 2019.
  4. ^ Hellgren, George (1960). "Något om växtligheten i Ydre". In Filén, Thure (ed.). Ydre-Boken (in Swedish). Linköping. pp. 86–91.{{cite book}}: CS1 maint: location missing publisher (link)
  5. ^ a b Enright, Kelly (5 October 2022). "Dreaming of Rediscovery: Botanists, Extinction, and the Tree That Sets the Brain on Fire". Environmental History. 27 (4): 665–691. doi:10.1086/721071.
  6. ^ a b Williams, Kevan (September 2014). "Have Tree, Will Travel". Landscape Architecture Magazine. 104 (9): 50, 52, 54, 56, 58. JSTOR 44796081 – via JSTOR.


Kembali kehalaman sebelumnya