Last Glacial Maximum

E179498

The Last Glacial Maximum was the most recent period in Earth’s history when ice sheets reached their greatest extent, dramatically lowering sea levels and reshaping global climates and ecosystems.

All labels observed (4)

Label Occurrences
Last Glacial Maximum canonical 21
Last Glacial Maximum cryosphere 1
Last Glacial Period 1

How this entity was disambiguated

Statements (52)

Predicate Object
instanceOf Quaternary climatic phase ⓘ
glacial maximum ⓘ
paleoclimatic event ⓘ
alsoKnownAs LGM ⓘ
linked to: Würm glaciation
associatedWith lower atmospheric CO2 concentrations ⓘ
causedExposureOf Bering Land Bridge ⓘ
Doggerland in the North Sea ⓘ
linked to: North Sea

Sahul Shelf land areas ⓘ
linked to: Sahul Shelf

Sunda Shelf land areas ⓘ
linked to: Sunda Shelf
characterizedBy altered global atmospheric circulation ⓘ
altered ocean circulation patterns ⓘ
colder global temperatures ⓘ
drier conditions in many regions ⓘ
expanded deserts and semi-arid regions ⓘ
expanded mountain glaciers worldwide ⓘ
large continental ice sheets over Asia ⓘ
large continental ice sheets over North America ⓘ
large continental ice sheets over northern Europe ⓘ
lower global sea level ⓘ
maximum global ice-sheet extent in the late Pleistocene ⓘ
followedBy deglaciation of the last glacial period ⓘ
transition to the Holocene ⓘ
hasApproximateCO2Concentration about 180 to 190 ppm ⓘ
hasApproximateEnd about 19,000 to 20,000 years ago ⓘ
hasApproximateStart about 26,500 years ago ⓘ
hasEstimatedGlobalMeanTemperatureChange about 4 to 7 degrees Celsius cooler than preindustrial ⓘ
hasEstimatedGlobalSeaLevelChange about 120 to 130 meters lower than present ⓘ
hasKeyProxy dust concentrations in ice cores ⓘ
foraminifera assemblages ⓘ
oxygen isotope ratios ⓘ
hasMajorIceSheet Barents–Kara Ice Sheet ⓘ
British–Irish Ice Sheet ⓘ
Cordilleran Ice Sheet ⓘ
East Antarctic Ice Sheet ⓘ
Fennoscandian Ice Sheet ⓘ
Greenland Ice Sheet ⓘ
Laurentide Ice Sheet ⓘ
Patagonian Ice Sheet ⓘ
West Antarctic Ice Sheet ⓘ
linked to: West Antarctica
hasPeakAround about 21,000 years ago ⓘ
impacted distribution of plant and animal species ⓘ
global ecosystems ⓘ
human migration routes ⓘ
partOf Last Glacial Period ⓘ
Pleistocene epoch ⓘ
Quaternary period ⓘ
precededBy earlier Pleistocene glacial maxima ⓘ
studiedUsing glacial geomorphological evidence ⓘ
ice core records ⓘ
marine sediment cores ⓘ
pollen and plant macrofossils ⓘ
terrestrial sediment records ⓘ

How these facts were elicited

Referenced by (24)

Full triples — surface form annotated when it differs from this entity's canonical label.

Quaternary period → contains → Last Glacial Maximum ⓘ
Wisconsin glaciation → maximumIceExtentReached → Last Glacial Maximum ⓘ
Bering Land Bridge → mostRecentExposure → Last Glacial Maximum ⓘ
Holocene climatic optimum → follows → Last Glacial Period ⓘ
linked to: Last Glacial Maximum
Fennoscandian Ice Sheet → lastMaximum → Last Glacial Maximum ⓘ
Yoldiahavet → formedAfter → Last Glacial Maximum ⓘ
subject linked to: Yoldiahavet (Swedish)
Yoldiahavet → formedAfter → Weichselian glaciation ⓘ
subject linked to: Yoldiahavet (Swedish)
linked to: Last Glacial Maximum
Sahul Shelf → exposedDuring → Last Glacial Maximum ⓘ
Beringian standstill hypothesis → timePeriod → Last Glacial Maximum ⓘ
Glacial Lake Columbia → formedDuring → Last Glacial Maximum ⓘ
British–Irish Ice Sheet → timePeriod → Last Glacial Maximum ⓘ
Yoldia stage → timeAfter → Last Glacial Maximum ⓘ
Solutrean archaeological culture → climateContext → Last Glacial Maximum ⓘ
Last Glacial Period → hasPhase → Last Glacial Maximum ⓘ
Last Glacial Period → hasPeak → Last Glacial Maximum ⓘ
Barents–Kara Ice Sheet → partOf → Last Glacial Maximum cryosphere ⓘ
linked to: Last Glacial Maximum
Barents–Kara Ice Sheet → existedDuring → Last Glacial Maximum ⓘ
Holocene Baltic Sea stages → startAfter → Last Glacial Maximum ⓘ
Sahul landmass → timePeriod → Last Glacial Maximum ⓘ
ice-free corridor hypothesis → temporalContext → Last Glacial Maximum ⓘ
Puget Lobe → lastMajorAdvanceDuring → Last Glacial Maximum ⓘ
Pleistocene glaciation → includes → Last Glacial Maximum ⓘ