CM-013

Last Glacial Maximum

Large ice sheets, lower global mean sea level, and transformed habitats reshaped coastlines and human opportunities, while local timing and climate varied.

Period or EventTopic PageNot a Claim
When
~26,500–19,000 years ago
Where
Global ice-volume interval with regionally varied conditions
Sources
7
Last reviewed
2026-08-11

Overview

WHAT IT IS

Last Glacial Maximum

Large ice sheets, lower global mean sea level, and transformed habitats reshaped coastlines and human opportunities, while local timing and climate varied.

WHAT THE RECORD CONTAINS

Evidence on this page

  • Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: https://doi.org/10.1073/pnas.1411762111. Role: global sea-level/ice-volume reconstruction and GIA context.
  • Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: https://doi.org/10.1038/s41586-020-2617-x. Role: proxy-assimilated global mean cooling and climate sensitivity.
  • Seltzer, Alan M., et al. (2021). “Widespread six degrees Celsius cooling on land during the Last Glacial Maximum.” _Nature_ 593: 228–232. DOI: https://doi.org/10.1038/s41586-021-03467-6. Role: independent terrestrial paleotemperature evidence from groundwater noble gases.
WHERE INTERPRETATION BEGINS

Important limits

  • Bibliographic verification does not by itself establish that the full text was read.
  • The evidence does not automatically support broader causal, technological, transmission, or literalizing claims beyond the cited record.

Current assessment

Not a Claim

This assessment belongs to this record only. A connection never transfers evidence status from another topic.

Source foundation

7 public source records are linked to this topic. Source quantity does not replace source quality or methodological review.

  • 6 Academic
  • 1 Institutional

6 academic-paper records · 1 with explicit free-full-text or open-access status

Evidence and claims

Recorded claims

CM-013-CL-001

During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.

SOURCE OR EVIDENCE RECORD

What the cited material supports

Global land-ice volume was near its last-cycle maximum and mean sea level was far below present.

Canonical sources cited

MODERN CLAIM OR INTERPRETATION

During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.

Well supported
Claim type
historical/textual/scientific/interpretive claim; see canonical record context
Origin / claimant
Installed canonical dossier and its cited source trail
Earliest recorded appearance
See Source Spine and claim-source comparison; exact origin retained where documented.
Last reviewed
2026-08-10

Where the interpretations diverge

See Internet Folklore and Claim Mutation section.

What the cited evidence does not establish

The evidence does not automatically support broader causal, technological, transmission, or literalizing claims beyond the cited record.
Follow the claim source trail

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

CM-013-CL-002

Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.

SOURCE OR EVIDENCE RECORD

What the cited material supports

Ice thickness, regional onset and retreat, rapid sea-level episodes, and local relative sea-level histories.

Canonical sources cited

MODERN CLAIM OR INTERPRETATION

Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.

Active debate
Claim type
historical/textual/scientific/interpretive claim; see canonical record context
Origin / claimant
Installed canonical dossier and its cited source trail
Earliest recorded appearance
See Source Spine and claim-source comparison; exact origin retained where documented.
Last reviewed
2026-08-10

Where the interpretations diverge

See Internet Folklore and Claim Mutation section.

What the cited evidence does not establish

The evidence does not automatically support broader causal, technological, transmission, or literalizing claims beyond the cited record.
Follow the claim source trail

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

Evidence Ledger

CM-013-EV-002

Lambeck, Kurt, et al

Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: https://doi.org/10.1073/pnas.1411762111. Role: global sea-level/ice-volume reconstruction and GIA context.

Evidence ID
CM-013-EV-002
Source records
1
Supports claims
1
Challenges claims
0

What this supports

  • During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.

What this does not establish

Bibliographic verification does not by itself establish that the full text was read.

Follow the Source

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

CM-013-EV-003

Tierney, Jessica E

Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: https://doi.org/10.1038/s41586-020-2617-x. Role: proxy-assimilated global mean cooling and climate sensitivity.

Evidence ID
CM-013-EV-003
Source records
1
Supports claims
0
Challenges claims
0

What this supports

No direct public claim-support relationship is recorded for this evidence item.

What this does not establish

Bibliographic verification does not by itself establish that the full text was read.

Follow the Source

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

CM-013-EV-004

Seltzer, Alan M

Seltzer, Alan M., et al. (2021). “Widespread six degrees Celsius cooling on land during the Last Glacial Maximum.” _Nature_ 593: 228–232. DOI: https://doi.org/10.1038/s41586-021-03467-6. Role: independent terrestrial paleotemperature evidence from groundwater noble gases.

Evidence ID
CM-013-EV-004
Source records
1
Supports claims
0
Challenges claims
0

What this supports

No direct public claim-support relationship is recorded for this evidence item.

What this does not establish

Bibliographic verification does not by itself establish that the full text was read.

Follow the Source

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

CM-013-EV-005

Gowan, Evan J

Gowan, Evan J., et al. (2021). “A new global ice sheet reconstruction for the past 80,000 years.” _Nature Communications_ 12. DOI: https://doi.org/10.1038/s41467-021-21469-w. Role: PaleoMIST 1.0 reconstruction and ice-volume uncertainty.

Evidence ID
CM-013-EV-005
Source records
1
Supports claims
2
Challenges claims
0

What this supports

  • During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.
  • Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.

What this does not establish

Bibliographic verification does not by itself establish that the full text was read.

Follow the Source

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

CM-013-EV-006

Purcell, Anthony, et al

Purcell, Anthony, et al. (2016). “An assessment of the ICE-6G_C (VM5a) glacial isostatic adjustment model.” _Journal of Geophysical Research: Solid Earth_. DOI: https://doi.org/10.1002/2015JB012742. Role: model assessment; explains why local relative sea level differs from a global bathtub map.

Evidence ID
CM-013-EV-006
Source records
1
Supports claims
2
Challenges claims
0

What this supports

  • During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.
  • Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.

What this does not establish

Bibliographic verification does not by itself establish that the full text was read.

Follow the Source

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

CM-013-EV-007

NOAA National Centers for Environmental Information, Paleoclimatology

NOAA National Centers for Environmental Information, Paleoclimatology. https://www.ncei.noaa.gov/products/paleoclimatology. Role: institutional data archive and proxy-data access, not a substitute for claim-specific papers.

Evidence ID
CM-013-EV-007
Source records
1
Supports claims
0
Challenges claims
0

What this supports

No direct public claim-support relationship is recorded for this evidence item.

What this does not establish

Bibliographic verification does not by itself establish that the full text was read.

Follow the Source

This trail lists canonical source records attached to this item. Display order does not imply evidentiary rank or historical sequence.

View as Evidence Matrix

Each row remains a separate evidence record. One proxy or finding does not automatically determine the assessment of an entire compound claim.

Structured evidence matrix
IDEvidenceSupportsChallengesMain limitationSources
CM-013-EV-002Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: https://doi.org/10.1073/pnas.1411762111. Role: global sea-level/ice-volume reconstruction and GIA context.During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.No direct public challenge relationship recordedBibliographic verification does not by itself establish that the full text was read.1
CM-013-EV-003Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: https://doi.org/10.1038/s41586-020-2617-x. Role: proxy-assimilated global mean cooling and climate sensitivity.No direct public support relationship recordedNo direct public challenge relationship recordedBibliographic verification does not by itself establish that the full text was read.1
CM-013-EV-004Seltzer, Alan M., et al. (2021). “Widespread six degrees Celsius cooling on land during the Last Glacial Maximum.” _Nature_ 593: 228–232. DOI: https://doi.org/10.1038/s41586-021-03467-6. Role: independent terrestrial paleotemperature evidence from groundwater noble gases.No direct public support relationship recordedNo direct public challenge relationship recordedBibliographic verification does not by itself establish that the full text was read.1
CM-013-EV-005Gowan, Evan J., et al. (2021). “A new global ice sheet reconstruction for the past 80,000 years.” _Nature Communications_ 12. DOI: https://doi.org/10.1038/s41467-021-21469-w. Role: PaleoMIST 1.0 reconstruction and ice-volume uncertainty.During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.; Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.No direct public challenge relationship recordedBibliographic verification does not by itself establish that the full text was read.1
CM-013-EV-006Purcell, Anthony, et al. (2016). “An assessment of the ICE-6G_C (VM5a) glacial isostatic adjustment model.” _Journal of Geophysical Research: Solid Earth_. DOI: https://doi.org/10.1002/2015JB012742. Role: model assessment; explains why local relative sea level differs from a global bathtub map.During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.; Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.No direct public challenge relationship recordedBibliographic verification does not by itself establish that the full text was read.1
CM-013-EV-007NOAA National Centers for Environmental Information, Paleoclimatology. https://www.ncei.noaa.gov/products/paleoclimatology. Role: institutional data archive and proxy-data access, not a substitute for claim-specific papers.No direct public support relationship recordedNo direct public challenge relationship recordedBibliographic verification does not by itself establish that the full text was read.1

Timeline

archaeological

~26,500–19,000 years ago

Approximate ordering never replaces this visible date basis.

archaeological

Before 30,000 years ago: The world moves toward full glacial conditions; ice sheets and glaciers expand unevenly.

Approximate ordering never replaces this visible date basis.

Open global timeline

Local Atlas Map

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This is a node-and-connection knowledge graph. Node distance is not evidence. Zoom or pan to separate dense areas.
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Accessible local relationship list
CM-012-CN-002

Last Glacial Maximum → Paleolithic Period

chronologystrong
This topic is related to CM-012 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-012-CN-002
Relationship
Chronology
Subtype
Chronology
Strength
strong
Direction
bidirectional
Evidence basis
AT-0099 places the Last Glacial Maximum at about 26.5–19 ka, a late interval within the much longer Paleolithic record.
Last reviewed
2026-08-10

What this does not prove

Chronological overlap does not imply one uniform environment, technology, population history, or cultural response across Paleolithic regions.

Supporting sources: Peter U. Clark et al. (2009), “The Last Glacial Maximum.” Science. DOI: https://doi.org/10.1126/science.1172873 — 26.5–19 ka global ice-volume synthesis.

Open Paleolithic PeriodCompare Carefully
CM-022-CN-001

Last Glacial Maximum → White Sands Footprints

chronologystrong
This topic is related to CM-022 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-022-CN-001
Relationship
Chronology
Subtype
Chronology
Strength
strong
Direction
bidirectional
Evidence basis
Independent seed, pollen, and luminescence chronologies place the White Sands track-bearing depositional sequence within Last Glacial Maximum times.
Last reviewed
2026-08-10

What this does not prove

This dates the containing sequence broadly to the LGM; it does not directly date every footprint or determine migration route or ancestry.

Supporting sources: Bennett, Matthew R., et al. (2021). “Evidence of humans in North America during the Last Glacial Maximum.” _Science_ 373(6562): 1528–1531. DOI: https://doi.org/10.1126/science.abg7586. Role: original high-profile track and seed chronology., Pigati, Jeffrey S., et al. (2023). “Independent age estimates resolve the controversy of ancient human footprints at White Sands.” _Science_ 382(6666): 73–75. DOI: https://doi.org/10.1126/science.adh5007. Role: terrestrial pollen radiocarbon and OSL confirmation., Holliday, Vance T., et al. (2025). “Paleolake geochronology supports Last Glacial Maximum (LGM) age for human tracks at White Sands, New Mexico.” _Science Advances_ 11(25). DOI: https://doi.org/10.1126/sciadv.adv4951. Role: independent stratigraphic/paleolake chronology and 26 additional radiocarbon dates.

Open White Sands FootprintsCompare Carefully
CM-025-CN-001

Last Glacial Maximum → Younger Dryas Impact Hypothesis

chronologystrong
This topic is related to CM-025 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-025-CN-001
Relationship
Chronology
Subtype
Timeline transition
Strength
strong
Direction
bidirectional
Evidence basis
The Younger Dryas onset postdates the Last Glacial Maximum by millennia and belongs to a later deglacial climate interval.
Last reviewed
2026-08-10

What this does not prove

This chronological relationship neither establishes an extraterrestrial trigger nor makes the LGM and Younger Dryas the same event.

Supporting sources: Pinter, Nicholas, et al. (2011). “The Younger Dryas impact hypothesis: A requiem.” _Earth-Science Reviews_ 106: 247–264. DOI: https://doi.org/10.1016/j.earscirev.2011.02.005. Role: early multidisciplinary critical synthesis., Holliday, Vance T., et al. (2023). “Comprehensive refutation of the Younger Dryas Impact Hypothesis.” _Earth-Science Reviews_ 247: 104502. DOI: https://doi.org/10.1016/j.earscirev.2023.104502. Role: current central critical review.

Open Younger Dryas Impact HypothesisCompare Carefully
CM-030-CN-001

Last Glacial Maximum → Meltwater Pulse 1A

chronologystrong
This topic is related to CM-030 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-030-CN-001
Relationship
Chronology
Subtype
Deglaciation
Strength
strong
Direction
bidirectional
Evidence basis
Meltwater Pulse 1A occurred during deglaciation after the Last Glacial Maximum and represents rapid global mean sea-level rise over several centuries.
Last reviewed
2026-08-10

What this does not prove

Rapid multi-century rise is not an instantaneous global flood and does not identify one ice-sheet source with certainty.

Supporting sources: Fairbanks (1989), 17,000-year glacio-eustatic sea-level record, Clark et al. (2002), sea-level fingerprinting and Meltwater Pulse 1A, Deschamps et al. (2012), ice-sheet collapse and sea-level rise at Bølling warming, Lin et al. (2021), reconciled Meltwater Pulse 1A sources

Open Meltwater Pulse 1ACompare Carefully
CM-023-CN-001

Last Glacial Maximum → Bering Land Bridge

geographystrong
This topic is related to CM-023 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-023-CN-001
Relationship
Geography and site network
Subtype
Paleogeography
Strength
strong
Direction
bidirectional
Evidence basis
Low glacial sea level exposed the Bering platform, while paleoecological evidence describes Beringia as a connected terrestrial ecosystem.
Last reviewed
2026-08-10

What this does not prove

Land exposure establishes paleogeographic connectivity, not a single migration date, route south of the ice sheets, or one demographic event.

Supporting sources: Hoffecker et al. (2016), Beringia and the Global Dispersal of Modern Humans, Wanket et al. (2025), Converging evidence constrains Late Pleistocene Bering Land Bridge history

Open Bering Land BridgeCompare Carefully
CM-013-CN-001

Last Glacial Maximum → Paleolithic Period

chronologymoderate
The Last Glacial Maximum transformed environments during one late portion of the much longer Paleolithic record.
Inspect connection as text
Connection ID
CM-013-CN-001
Relationship
Chronology
Subtype
Chronology
Strength
moderate
Direction
bidirectional
Evidence basis
The Last Glacial Maximum is a late-Pleistocene interval whose independently reconstructed climate and sea-level conditions provide chronology context for late Paleolithic records.
Last reviewed
2026-08-10

What this does not prove

The edge supplies environmental chronology only; it does not establish uniform human behavior, migration, or cultural causation.

Supporting sources: Clark, Peter U., et al. (2009). “The Last Glacial Maximum.” _Science_ 325(5941): 710–714. DOI: https://doi.org/10.1126/science.1172873. Role: standard chronological and conceptual synthesis., Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: https://doi.org/10.1073/pnas.1411762111. Role: global sea-level/ice-volume reconstruction and GIA context., Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: https://doi.org/10.1038/s41586-020-2617-x. Role: proxy-assimilated global mean cooling and climate sensitivity.

Open Paleolithic PeriodCompare Carefully
Open full Atlas Map

Documented connections

CM-012-CN-002

Last Glacial Maximum → Paleolithic Period

chronologystrong
This topic is related to CM-012 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-012-CN-002
Relationship
Chronology
Subtype
Chronology
Strength
strong
Direction
bidirectional
Evidence basis
AT-0099 places the Last Glacial Maximum at about 26.5–19 ka, a late interval within the much longer Paleolithic record.
Last reviewed
2026-08-10

What this does not prove

Chronological overlap does not imply one uniform environment, technology, population history, or cultural response across Paleolithic regions.

Supporting sources: Peter U. Clark et al. (2009), “The Last Glacial Maximum.” Science. DOI: https://doi.org/10.1126/science.1172873 — 26.5–19 ka global ice-volume synthesis.

Open Paleolithic PeriodCompare Carefully
CM-022-CN-001

Last Glacial Maximum → White Sands Footprints

chronologystrong
This topic is related to CM-022 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-022-CN-001
Relationship
Chronology
Subtype
Chronology
Strength
strong
Direction
bidirectional
Evidence basis
Independent seed, pollen, and luminescence chronologies place the White Sands track-bearing depositional sequence within Last Glacial Maximum times.
Last reviewed
2026-08-10

What this does not prove

This dates the containing sequence broadly to the LGM; it does not directly date every footprint or determine migration route or ancestry.

Supporting sources: Bennett, Matthew R., et al. (2021). “Evidence of humans in North America during the Last Glacial Maximum.” _Science_ 373(6562): 1528–1531. DOI: https://doi.org/10.1126/science.abg7586. Role: original high-profile track and seed chronology., Pigati, Jeffrey S., et al. (2023). “Independent age estimates resolve the controversy of ancient human footprints at White Sands.” _Science_ 382(6666): 73–75. DOI: https://doi.org/10.1126/science.adh5007. Role: terrestrial pollen radiocarbon and OSL confirmation., Holliday, Vance T., et al. (2025). “Paleolake geochronology supports Last Glacial Maximum (LGM) age for human tracks at White Sands, New Mexico.” _Science Advances_ 11(25). DOI: https://doi.org/10.1126/sciadv.adv4951. Role: independent stratigraphic/paleolake chronology and 26 additional radiocarbon dates.

Open White Sands FootprintsCompare Carefully
CM-025-CN-001

Last Glacial Maximum → Younger Dryas Impact Hypothesis

chronologystrong
This topic is related to CM-025 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-025-CN-001
Relationship
Chronology
Subtype
Timeline transition
Strength
strong
Direction
bidirectional
Evidence basis
The Younger Dryas onset postdates the Last Glacial Maximum by millennia and belongs to a later deglacial climate interval.
Last reviewed
2026-08-10

What this does not prove

This chronological relationship neither establishes an extraterrestrial trigger nor makes the LGM and Younger Dryas the same event.

Supporting sources: Pinter, Nicholas, et al. (2011). “The Younger Dryas impact hypothesis: A requiem.” _Earth-Science Reviews_ 106: 247–264. DOI: https://doi.org/10.1016/j.earscirev.2011.02.005. Role: early multidisciplinary critical synthesis., Holliday, Vance T., et al. (2023). “Comprehensive refutation of the Younger Dryas Impact Hypothesis.” _Earth-Science Reviews_ 247: 104502. DOI: https://doi.org/10.1016/j.earscirev.2023.104502. Role: current central critical review.

Open Younger Dryas Impact HypothesisCompare Carefully
CM-030-CN-001

Last Glacial Maximum → Meltwater Pulse 1A

chronologystrong
This topic is related to CM-030 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-030-CN-001
Relationship
Chronology
Subtype
Deglaciation
Strength
strong
Direction
bidirectional
Evidence basis
Meltwater Pulse 1A occurred during deglaciation after the Last Glacial Maximum and represents rapid global mean sea-level rise over several centuries.
Last reviewed
2026-08-10

What this does not prove

Rapid multi-century rise is not an instantaneous global flood and does not identify one ice-sheet source with certainty.

Supporting sources: Fairbanks (1989), 17,000-year glacio-eustatic sea-level record, Clark et al. (2002), sea-level fingerprinting and Meltwater Pulse 1A, Deschamps et al. (2012), ice-sheet collapse and sea-level rise at Bølling warming, Lin et al. (2021), reconciled Meltwater Pulse 1A sources

Open Meltwater Pulse 1ACompare Carefully
CM-023-CN-001

Last Glacial Maximum → Bering Land Bridge

geographystrong
This topic is related to CM-023 for the same bounded reason; reciprocal wording does not add a stronger causal claim.
Inspect connection as text
Connection ID
CM-023-CN-001
Relationship
Geography and site network
Subtype
Paleogeography
Strength
strong
Direction
bidirectional
Evidence basis
Low glacial sea level exposed the Bering platform, while paleoecological evidence describes Beringia as a connected terrestrial ecosystem.
Last reviewed
2026-08-10

What this does not prove

Land exposure establishes paleogeographic connectivity, not a single migration date, route south of the ice sheets, or one demographic event.

Supporting sources: Hoffecker et al. (2016), Beringia and the Global Dispersal of Modern Humans, Wanket et al. (2025), Converging evidence constrains Late Pleistocene Bering Land Bridge history

Open Bering Land BridgeCompare Carefully
CM-013-CN-001

Last Glacial Maximum → Paleolithic Period

chronologymoderate
The Last Glacial Maximum transformed environments during one late portion of the much longer Paleolithic record.
Inspect connection as text
Connection ID
CM-013-CN-001
Relationship
Chronology
Subtype
Chronology
Strength
moderate
Direction
bidirectional
Evidence basis
The Last Glacial Maximum is a late-Pleistocene interval whose independently reconstructed climate and sea-level conditions provide chronology context for late Paleolithic records.
Last reviewed
2026-08-10

What this does not prove

The edge supplies environmental chronology only; it does not establish uniform human behavior, migration, or cultural causation.

Supporting sources: Clark, Peter U., et al. (2009). “The Last Glacial Maximum.” _Science_ 325(5941): 710–714. DOI: https://doi.org/10.1126/science.1172873. Role: standard chronological and conceptual synthesis., Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: https://doi.org/10.1073/pnas.1411762111. Role: global sea-level/ice-volume reconstruction and GIA context., Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: https://doi.org/10.1038/s41586-020-2617-x. Role: proxy-assimilated global mean cooling and climate sensitivity.

Open Paleolithic PeriodCompare Carefully

Sources

Academic papers

6 paper citations support or limit this topic; 1 carry explicit free-full-text or open-access status.

Academic

AT-0102

Clark, Peter U., et al. (2009). “The Last Glacial Maximum.” _Science_ 325(5941): 710–714. DOI: https://doi.org/10.1126/science.1172873. Role: standard chronological and conceptual synthesis.

Type
DOI
Verification
verified
Access
unavailable-through-registered-public-or-tdm-routes
Rights
not identified; not cleared
Retraction / correction
no retraction flag in checked Crossref/OpenAlex metadata

Why Ancient Inquiry uses this source

standard chronological and conceptual synthesis.

What it does not establish

Bibliographic verification does not by itself establish that the full text was read.

Linked academic citation
AT-0103

Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: https://doi.org/10.1073/pnas.1411762111. Role: global sea-level/ice-volume reconstruction and GIA context.

Type
DOI
Verification
verified
Access
unavailable-through-registered-public-or-tdm-routes
Rights
not identified; not cleared
Retraction / correction
no retraction flag in checked Crossref/OpenAlex metadata

Why Ancient Inquiry uses this source

global sea-level/ice-volume reconstruction and GIA context.

What it does not establish

Bibliographic verification does not by itself establish that the full text was read.

Linked academic citation
AT-0104

Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: https://doi.org/10.1038/s41586-020-2617-x. Role: proxy-assimilated global mean cooling and climate sensitivity.

Type
DOI
Verification
verified
Access
unavailable-through-registered-public-or-tdm-routes
Rights
https://www.springer.com/tdm; https://www.springer.com/tdm; not cleared
Retraction / correction
no retraction flag in checked Crossref/OpenAlex metadata

Why Ancient Inquiry uses this source

proxy-assimilated global mean cooling and climate sensitivity.

What it does not establish

Bibliographic verification does not by itself establish that the full text was read.

Linked academic citation
AT-0105

Seltzer, Alan M., et al. (2021). “Widespread six degrees Celsius cooling on land during the Last Glacial Maximum.” _Nature_ 593: 228–232. DOI: https://doi.org/10.1038/s41586-021-03467-6. Role: independent terrestrial paleotemperature evidence from groundwater noble gases.

Type
DOI
Verification
verified
Access
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independent terrestrial paleotemperature evidence from groundwater noble gases.

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AT-0106

Gowan, Evan J., et al. (2021). “A new global ice sheet reconstruction for the past 80,000 years.” _Nature Communications_ 12. DOI: https://doi.org/10.1038/s41467-021-21469-w. Role: PaleoMIST 1.0 reconstruction and ice-volume uncertainty.

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PaleoMIST 1.0 reconstruction and ice-volume uncertainty.

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Free full text
AT-0107

Purcell, Anthony, et al. (2016). “An assessment of the ICE-6G_C (VM5a) glacial isostatic adjustment model.” _Journal of Geophysical Research: Solid Earth_. DOI: https://doi.org/10.1002/2015JB012742. Role: model assessment; explains why local relative sea level differs from a global bathtub map.

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model assessment; explains why local relative sea level differs from a global bathtub map.

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NOAA National Centers for Environmental Information, Paleoclimatology. https://www.ncei.noaa.gov/products/paleoclimatology. Role: institutional data archive and proxy-data access, not a substitute for claim-specific papers.

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Why Ancient Inquiry uses this source

institutional data archive and proxy-data access, not a substitute for claim-specific papers.

What it does not establish

Bibliographic verification does not by itself establish that the full text was read.

Research detail

Topic ID: CM-013 Last reviewed: 2026-08-10 Corrections: /corrections/ Change history: Recorded in the Connected Atlas topic changelog.

Overview

Large ice sheets, lower global mean sea level, and transformed habitats reshaped coastlines and human opportunities, while local timing and climate varied.

Plain-language explanation

Between about 26,500 and 19,000 years ago, more water was stored in land ice. Global mean sea level was roughly 120–130 metres below present, but local shorelines differed because land and gravity respond to ice loading.

Historical and scholarly context

What the LGM was

The LGM was not the whole Ice Age. It was the maximum phase of the last glacial cycle. The Pleistocene had many cold and warm intervals, and the LGM was the most recent major cold maximum before the Holocene.

Sea level and exposed land

Because water was locked in ice sheets, global sea level was far lower than today. USGS summaries put global sea level around 125 meters below today at the LGM. This exposed parts of the continental shelf, including land and coastal plains that later disappeared under rising seas.

Climate and ecosystems

Global mean cooling was substantial, but not uniform. Tierney and colleagues reconstructed about 6.1 degrees Celsius of global mean cooling relative to preindustrial climate, while Seltzer and colleagues found widespread cooling of about six degrees Celsius on land using noble gases in ancient groundwater. Regional conditions could be colder, drier, windier, or ecologically different depending on location.

Human survival and migration

Humans were already widespread before and during the LGM. The cold maximum affected where people could live, which resources were available, and which routes were open. Some regions became refugia. Other regions became barriers. Beringia, exposed continental shelves, and coastal migration routes are especially important to the Americas discussion.

The flood-myth connection

The LGM connects to flood myths indirectly. The LGM lowered sea level. After the LGM, warming and ice melt raised sea level and sometimes produced dramatic local flooding. That later deglacial process could contribute to regional flood memories in some cases, but it does not prove a single global flood or one universal flood story.

What the evidence supports

The strongest evidence for the LGM comes from multiple independent records: ice cores, marine sediments, glacial landforms, sea-level indicators, climate proxies, and model reconstructions. The same broad pattern appears across different methods: colder climate, larger ice sheets, lower sea level, altered habitats, and later deglacial change.

The strongest story connection is not “a global flood.” It is the real fact that post-LGM sea-level rise drowned landscapes that humans may have used. That gives the LGM high connection value for migration, lost-coastline, and flood-memory topics without requiring unsupported conclusions.

Limits and disputed claims

  • Treating the LGM as a sudden global flood is incorrect.
  • Treating all flood myths as memories of post-LGM sea-level rise is overconfident.
  • Treating submerged land as proof of lost civilization is a weak argument without artifacts and dates.
  • Using modern coastlines to judge Paleolithic migration routes is misleading because coastlines changed dramatically.
  • Blending the LGM, Meltwater Pulse 1A, Younger Dryas, Storegga Slide, Black Sea Deluge, and Noah-style stories into one event creates a chronology problem.
  • Viral sea-level maps often omit uncertainty, dating, regional sea-level differences, and glacial isostatic adjustment.

Claim status

  • Well supported: During the Last Glacial Maximum, global land-ice volume was near its last-glacial-cycle maximum and global mean sea level was far below present.
  • Active debate: Reconstructions of regional Last Glacial Maximum ice thickness and local relative sea-level histories remain model-dependent.

Sources

  • Clark, Peter U., et al. (2009). “The Last Glacial Maximum.” _Science_ 325(5941): 710–714. DOI: <https://doi.org/10.1126/science.1172873>. Role: standard chronological and conceptual synthesis. — https://doi.org/10.1126/science.1172873
  • Lambeck, Kurt, et al. (2014). “Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.” _PNAS_ 111(43): 15296–15303. DOI: <https://doi.org/10.1073/pnas.1411762111>. Role: global sea-level/ice-volume reconstruction and GIA context. — https://doi.org/10.1073/pnas.1411762111
  • Tierney, Jessica E., et al. (2020). “Glacial cooling and climate sensitivity revisited.” _Nature_ 584: 569–573. DOI: <https://doi.org/10.1038/s41586-020-2617-x>. Role: proxy-assimilated global mean cooling and climate sensitivity. — https://doi.org/10.1038/s41586-020-2617-x
  • Seltzer, Alan M., et al. (2021). “Widespread six degrees Celsius cooling on land during the Last Glacial Maximum.” _Nature_ 593: 228–232. DOI: <https://doi.org/10.1038/s41586-021-03467-6>. Role: independent terrestrial paleotemperature evidence from groundwater noble gases. — https://doi.org/10.1038/s41586-021-03467-6
  • Gowan, Evan J., et al. (2021). “A new global ice sheet reconstruction for the past 80,000 years.” _Nature Communications_ 12. DOI: <https://doi.org/10.1038/s41467-021-21469-w>. Role: PaleoMIST 1.0 reconstruction and ice-volume uncertainty. — https://doi.org/10.1038/s41467-021-21469-w
  • Purcell, Anthony, et al. (2016). “An assessment of the ICE-6G_C (VM5a) glacial isostatic adjustment model.” _Journal of Geophysical Research: Solid Earth_. DOI: <https://doi.org/10.1002/2015JB012742>. Role: model assessment; explains why local relative sea level differs from a global bathtub map. — https://doi.org/10.1002/2015JB012742
  • NOAA National Centers for Environmental Information, Paleoclimatology. <https://www.ncei.noaa.gov/products/paleoclimatology>. Role: institutional data archive and proxy-data access, not a substitute for claim-specific papers. — https://www.ncei.noaa.gov/products/paleoclimatology

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