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4.2-kiloyear event Wiki2Web Clarity Challenge

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Study Guide: The 4.2 Kiloyear Event and the Meghalayan Age

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The 4.2 Kiloyear Event and the Meghalayan Age Study Guide

Defining the 4.2 ka Event and Meghalayan Age

The 4.2-kiloyear Before Present (BP) aridification event, commonly referred to as the 4.2 ka event, signifies the commencement of the Meghalayan age.

Answer: True

Explanation: The 4.2-kiloyear Before Present (BP) aridification event, designated as the 4.2 ka event, represents a significant climatic perturbation that commenced circa 2200 BC and persisted through the 22nd century BC. It is recognized as a pivotal climatic shift within the Holocene epoch and delineates the beginning of the Meghalayan age.

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The 4.2 ka event is recognized as a minor climatic shift within the Holocene epoch.

Answer: False

Explanation: The 4.2 ka event is recognized as one of the most significant climatic shifts during the Holocene epoch, not a minor one.

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The International Commission on Stratigraphy formally recognized the 4.2 ka event as the start of the Meghalayan age in 2018.

Answer: True

Explanation: The International Commission on Stratigraphy formalized the designation of the 4.2 ka event as the beginning of the Meghalayan age in 2018.

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What is the primary significance of the 4.2-kiloyear BP aridification event in geological time scales?

Answer: It defines the start of the Meghalayan age.

Explanation: The 4.2 ka event is significant as it formally defines the beginning of the Meghalayan age, the most recent geological age within the Holocene epoch.

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Which of the following is NOT listed as a significant climate event in the 'See also' section?

Answer: Little Ice Age

Explanation: The 'See also' section references the 8.2-kiloyear event, Bond events, and the mid-24th century BCE climate anomaly, among others, but does not list the Little Ice Age.

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Causes and Mechanisms of the 4.2 ka Event

A primary proposed cause for the 4.2 ka event is the weakening of the Atlantic meridional overturning circulation (AMOC).

Answer: True

Explanation: Modeling evidence suggests that a substantial weakening of the Atlantic meridional overturning circulation (AMOC) is a primary cause for the 4.2 ka event, disrupting global ocean currents and leading to climatic shifts.

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The weakening of the AMOC during the 4.2 ka event led to more stable global ocean currents.

Answer: False

Explanation: A weakening of the AMOC during the 4.2 ka event disrupted global ocean currents, leading to significant climatic changes, rather than stabilizing them.

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The Intertropical Convergence Zone (ITCZ) is believed to have shifted northward during the 4.2 ka event, causing aridification.

Answer: False

Explanation: The ITCZ is believed to have shifted southward during the 4.2 ka event, contributing to aridification in certain regions.

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Mesopotamian aridification during the 4.2 ka event is correlated with cooler sea-surface temperatures in the North Atlantic.

Answer: True

Explanation: Mesopotamian aridification during the 4.2 ka event is correlated with cooler sea-surface temperatures in the North Atlantic (Bond event 3), suggesting a teleconnection where reduced North Atlantic temperatures lead to decreased water supply in Mesopotamia.

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The Siberian High weakened during the 4.2 ka event, allowing more moisture into Central Asia.

Answer: False

Explanation: The Siberian High strengthened and increased in area during the 4.2 ka event, blocking westerly winds and causing intense aridification across Central Asia.

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The 4.2 ka event led to increased variability of the El Niño-Southern Oscillation (ENSO) in Borneo.

Answer: False

Explanation: In Borneo, the 4.2 ka event substantially reduced the variability of the El Niño-Southern Oscillation (ENSO), a reduction comparable only to the earlier 8.2 ka event.

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The 4.2 ka event is linked to the weakening of the Atlantic meridional overturning circulation (AMOC).

Answer: True

Explanation: A substantial weakening of the Atlantic meridional overturning circulation (AMOC) is considered a primary proposed cause for the 4.2 ka event, disrupting global ocean currents and leading to climatic changes.

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The southward shift of the ITCZ during the 4.2 ka event is proposed to be a consequence of increased solar activity.

Answer: False

Explanation: The southward shift of the ITCZ during the 4.2 ka event is proposed to be a consequence of the weakening of the Atlantic meridional overturning circulation (AMOC), not increased solar activity.

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Explosive volcanism in Iceland is considered a major confirmed cause of the 4.2 ka event.

Answer: False

Explanation: Explosive volcanism in Iceland has been proposed as a potential cause for the 4.2 ka event, but studies suggest its impact was likely negligible due to the low sulfur content of Icelandic volcanoes.

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What is considered a primary proposed cause for the 4.2 ka aridification event?

Answer: A substantial weakening of the Atlantic meridional overturning circulation (AMOC).

Explanation: A substantial weakening of the Atlantic meridional overturning circulation (AMOC) is considered a primary proposed cause for the 4.2 ka event, disrupting global ocean currents and leading to widespread climatic changes.

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How did the ITCZ's behavior contribute to the 4.2 ka event?

Answer: It shifted abruptly southward, influencing regional weather and contributing to aridification.

Explanation: The ITCZ is believed to have shifted abruptly southward during the 4.2 ka event, influencing regional weather patterns and contributing to the arid conditions experienced in certain areas.

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What impact did the 4.2 ka event have on ENSO variability in Borneo?

Answer: It substantially reduced ENSO variability.

Explanation: In Borneo, the 4.2 ka event substantially reduced the variability of the El Niño-Southern Oscillation (ENSO), a reduction comparable only to the earlier 8.2 ka event.

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What is the proposed link between Mesopotamian aridification and North Atlantic temperatures during the 4.2 ka event?

Answer: Cooler North Atlantic temperatures (Bond event 3) correlated with reduced Mesopotamian water supply.

Explanation: Mesopotamian aridification during the 4.2 ka event is correlated with cooler North Atlantic temperatures (Bond event 3), suggesting that reduced water supply in Mesopotamia is linked to cooler subpolar northwest Atlantic temperatures.

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What was the proposed reason for the southward shift of the ITCZ during the 4.2 ka event?

Answer: Weakening of the Atlantic meridional overturning circulation (AMOC).

Explanation: The southward shift of the Intertropical Convergence Zone (ITCZ) during the 4.2 ka event is proposed to be a consequence of the weakening of the Atlantic meridional overturning circulation (AMOC).

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What is the proposed role of Icelandic volcanism in the 4.2 ka event?

Answer: It was proposed as a potential cause, but likely had a negligible impact.

Explanation: Explosive volcanism in Iceland has been proposed as a potential cause for the 4.2 ka event; however, studies suggest that the low sulfur content of Icelandic volcanoes likely resulted in a negligible impact on global climate.

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Regional Impacts and Paleoclimatic Evidence

Evidence for the 4.2 ka event includes records of intense aridity in the Middle East and North Africa.

Answer: True

Explanation: Records of intense aridity in regions such as North Africa and the Middle East constitute key evidence supporting the occurrence of the 4.2 ka event.

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Glacial advances were observed in regions like western Canada and Iceland during the 4.2 ka event.

Answer: True

Explanation: Evidence for the 4.2 ka event includes observations of glacial advances in areas such as western Canada and Iceland.

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Evidence for the 4.2 ka event in the British Isles is considered clear and unambiguous.

Answer: False

Explanation: The evidence for the 4.2 ka event in the British Isles is considered ambiguous and unclear, with specific regional manifestations remaining uncertain.

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In Poland, sediment analysis indicates that winters became colder between 4250 and 4000 BP during the 4.2 ka event.

Answer: True

Explanation: Sediment analysis from Poland indicates colder winters between 4250 and 4000 BP, correlating with the 4.2 ka event, while summer temperatures remained constant and humidity was not significantly affected.

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The Iberian Peninsula experienced widespread aridification throughout the entire 4.2 ka event period.

Answer: False

Explanation: While the Iberian Peninsula experienced aridification phases, reconstructions indicate two distinct dry periods followed by wetter conditions, not widespread aridification throughout the entire event.

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The Gulf of Genoa experienced drier summers and cooler winters during the 4.2 ka event.

Answer: False

Explanation: The Gulf of Genoa experienced drier winters and wetter, cooler summers during the 4.2 ka event, contrary to the statement.

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The Alps experienced a wetter climate with increased precipitation during the ice-free season, according to isotopic data from Lake Petit.

Answer: True

Explanation: Isotopic data from Lake Petit indicates that the Alps experienced a wetter climate with increased precipitation during the ice-free season during the 4.2 ka event.

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Southern Italy experienced humidification during the 4.2 ka event, leading to forest expansion.

Answer: False

Explanation: Southern Italy experienced intense aridification during the 4.2 ka event, which led to a significant decline in forests, not expansion.

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In the Middle Atlas region of North Africa, speleothem analysis suggests a cooler and more humid climate during the 4.2 ka event.

Answer: True

Explanation: Speleothem analysis from the Middle Atlas region of North Africa indicates that the 4.2 ka event resulted in a cooler and more humid climate in that specific area.

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The south-central Levant experienced a consistent dry climate throughout the 4.2 ka event.

Answer: False

Explanation: In the south-central Levant, the 4.2 ka event is described as a 'W-shaped' event, characterized by two distinct dry phases separated by a wetter interval, not a consistent dry climate.

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Both the Indian Summer Monsoon (ISM) and Indian Winter Monsoon (IWM) strengthened during the 4.2 ka event.

Answer: False

Explanation: Both the Indian Summer Monsoon (ISM) and the Indian Winter Monsoon (IWM) experienced a decline in strength during the 4.2 ka event, leading to arid conditions.

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The East Asian Summer Monsoon (EASM) significantly strengthened during the 4.2 ka event.

Answer: False

Explanation: The East Asian Summer Monsoon (EASM) experienced an enormous reduction in strength during the 4.2 ka event, impacting rainfall patterns.

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Proxy records from Hulun Lake in Inner Mongolia show a major dry event in northeastern China between 4210 and 3840 BP.

Answer: True

Explanation: Proxy records from Hulun Lake in Inner Mongolia indicate a major dry event occurred in northeastern China between 4210 and 3840 BP, consistent with the 4.2 ka event.

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The Korean Peninsula experienced significant aridification during the 4.2 ka event, although Jeju Island remained humid.

Answer: True

Explanation: Significant aridification occurred on the Korean Peninsula during the 4.2 ka event, as evidenced by pollen data, although Jeju Island maintained a humid climate.

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Rebun Island, Japan, experienced an abrupt and intense cooling event around 4,130 BP, associated with the 4.2 ka event.

Answer: True

Explanation: Rebun Island, Japan, experienced an abrupt and intense cooling event around 4,130 BP, which is associated with the 4.2 ka event.

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Stalagmites in northeastern Namibia indicate that the region became drier due to the southward shift of the ITCZ during the 4.2 ka event.

Answer: False

Explanation: Stalagmites from northeastern Namibia indicate that the region became wetter due to the southward shift of the ITCZ during the 4.2 ka event, not drier.

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No signal of the 4.2 ka event has been found in Rodrigues.

Answer: True

Explanation: No evidence or signal related to the 4.2 ka event has been identified in Rodrigues.

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The image caption for the global distribution map indicates that dotted areas experienced wet conditions.

Answer: False

Explanation: The image caption specifies that dotted areas on the global distribution map represent regions affected by drought or dust storms, while hatched areas indicate wet conditions or flooding.

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The 4.2 ka event caused an increase in precipitation in Central China, according to Yonglu Cave records.

Answer: True

Explanation: According to records from Yonglu Cave in Hubei, Central China experienced an increase in precipitation during the 4.2 ka event, contrasting with aridification in many surrounding regions.

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The 4.2 ka event caused drier winters and wetter, cooler summers in the Gulf of Genoa.

Answer: True

Explanation: In the Gulf of Genoa, the 4.2 ka event resulted in drier winters and wetter, cooler summers, attributed to changes in atmospheric circulation patterns.

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The 4.2 ka event is associated with a decline in the abundance of the yew tree in eastern England.

Answer: True

Explanation: A decline in the abundance of the yew tree in eastern England has been noted and is associated with the climatic changes during the 4.2 ka event.

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Sediment records from Rara Lake indicate a strengthening of the Indian Summer Monsoon (ISM) during the 4.2 ka event.

Answer: False

Explanation: Sediment records from Rara Lake indicate a decline in the strength of the Indian Summer Monsoon (ISM) during the 4.2 ka event, evidenced by low Mn/Ti and Mn/Fe ratios.

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Which of the following is cited as evidence for the 4.2 ka event in North Africa?

Answer: Records of intense aridity

Explanation: Records of intense aridity in North Africa are cited as evidence for the 4.2 ka event. While the Middle Atlas region experienced cooler and more humid conditions, other parts of North Africa showed signs of drought.

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What was the climatic impact of the 4.2 ka event on the Iberian Peninsula?

Answer: Two distinct dry phases followed by wetter conditions.

Explanation: The Iberian Peninsula generally experienced stable conditions, but reconstructions show two distinct dry phases between approximately 2350-2200 BC and 2100-2000 BC, followed by wetter conditions.

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How did the climate change in the Gulf of Genoa during the 4.2 ka event?

Answer: Drier winters and cooler summers.

Explanation: In the Gulf of Genoa, the 4.2 ka event led to a drop in mean annual temperature, with winters becoming drier and summers wetter and cooler.

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What was the impact of the 4.2 ka event on the Indian monsoons?

Answer: Both ISM and IWM experienced a decline in strength.

Explanation: Both the Indian Summer Monsoon (ISM) and the Indian Winter Monsoon (IWM) experienced a decline in strength during the 4.2 ka event, leading to arid conditions in northwestern South Asia.

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How did the East Asian Summer Monsoon (EASM) change during the 4.2 ka event?

Answer: It experienced an enormous reduction in strength.

Explanation: The 4.2 ka event caused an enormous reduction in the strength of the East Asian Summer Monsoon (EASM), potentially due to the cooling of North Atlantic waters slowing its northward movement.

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What did stalagmites from northeastern Namibia indicate about the climate during the 4.2 ka event?

Answer: The region became wetter due to the southward shift of the ITCZ.

Explanation: Stalagmites from northeastern Namibia indicate that the region became wetter due to the southward shift of the ITCZ during the 4.2 ka event, with this humidification occurring in two distinct pulses.

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What impact did the 4.2 ka event have on the yew tree in eastern England?

Answer: It led to a decline in yew tree abundance.

Explanation: The 4.2 ka event is associated with a decline in the abundance of the yew tree in eastern England.

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What specific climate change occurred in northeastern China between 4210 and 3840 BP, according to records from Hulun Lake?

Answer: A major dry event.

Explanation: Proxy records from Hulun Lake in Inner Mongolia indicate a major dry event occurred in northeastern China between 4210 and 3840 BP, correlating with the 4.2 ka event.

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What do low manganese-to-titanium and manganese-to-iron ratios in Rara Lake sediment suggest about the Indian Summer Monsoon (ISM) during the 4.2 ka event?

Answer: A decline in the strength of the ISM.

Explanation: Low manganese-to-titanium and manganese-to-iron ratios in Rara Lake sediment during the 4.2 ka event are interpreted as evidence for a decline in the strength of the Indian Summer Monsoon (ISM).

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Which statement accurately reflects the impact of the 4.2 ka event on Central China, according to Yonglu Cave records?

Answer: Central China saw an increase in precipitation.

Explanation: According to Yonglu Cave records, Central China experienced an increase in precipitation during the 4.2 ka event, contrasting with the aridification observed in many surrounding regions.

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Civilizational Impacts and Societal Responses

The collapse of the Old Kingdom of Egypt is hypothesized to be linked to the 4.2 ka event.

Answer: True

Explanation: The 4.2 ka event is linked to exceptionally low Nile floods around 2150 BC, a factor hypothesized to have contributed to the collapse of Egypt's Old Kingdom.

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The Akkadian Empire in Mesopotamia is one of the ancient civilizations suggested to have been affected by the 4.2 ka event.

Answer: True

Explanation: The Akkadian Empire's collapse around 2300 BC is claimed to have been influenced by a widespread drought associated with the 4.2 ka event, leading to agricultural disruption and societal strain.

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The construction of 'motillas' in Spain is proposed as a response to the aridification caused by the 4.2 ka event.

Answer: True

Explanation: The construction of 'motillas,' ancient groundwater collection systems in Spain, is hypothesized as a direct response to the severe aridification associated with the 4.2 ka event.

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The 4.2 ka event is linked to exceptionally low Nile floods around 2150 BC, potentially contributing to the collapse of Egypt's Old Kingdom.

Answer: True

Explanation: The 4.2 ka event is associated with exceptionally low Nile floods around 2150 BC, a factor that may have contributed to the collapse of Egypt's Old Kingdom.

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The collapse of the Akkadian Empire is claimed to be unrelated to the 4.2 ka event's drought.

Answer: False

Explanation: The collapse of the Akkadian Empire is claimed to be influenced by a widespread drought associated with the 4.2 ka event, impacting agricultural lands and potentially weakening the empire.

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The 4.2 ka event led to the continuation of the Umm Al Nar culture in the Persian Gulf region.

Answer: False

Explanation: The 4.2 ka event marked a significant change in the Persian Gulf region, leading to the end of the Umm Al Nar culture and the transition to the Wadi Suq culture.

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Fossil corals from Oman suggest that prolonged winter 'shamal' seasons around 2200 BC contributed to the Akkadian Empire's collapse by causing field salinization.

Answer: True

Explanation: Fossil corals from Oman indicate that prolonged winter 'shamal' seasons around 2200 BC led to field salinization, a factor proposed to have contributed to the Akkadian Empire's collapse.

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Drought is considered a primary factor in the collapse of the Indus Valley Civilization, linked to the 4.2 ka event.

Answer: True

Explanation: Drought, linked to the 4.2 ka event and a weakening monsoon, is considered a primary factor contributing to the collapse of the Indus Valley Civilization.

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The Ghaggar-Hakra river system expanded significantly during the 4.2 ka event due to increased monsoon rainfall.

Answer: False

Explanation: Aridification during the 4.2 ka event reduced water supply to the Ghaggar-Hakra river system, causing it to retract, not expand, making inundation agriculture unsustainable.

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The 4.2 ka event is not believed to have impacted Neolithic cultures or specific cultures like the Longshan and Liangzhu in China.

Answer: False

Explanation: The drought associated with the 4.2 ka event is believed to have contributed to the collapse or decline of Neolithic cultures in China, including the Longshan and Liangzhu civilizations.

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The 4.2 ka event had a discernible impact on the spread of millet cultivation in China.

Answer: False

Explanation: The 4.2 ka event did not have a discernible impact on the spread of millet cultivation in China.

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The Sannai-Maruyama site in Japan experienced growth during the period of the 4.2 ka event.

Answer: False

Explanation: The Sannai-Maruyama site in Japan experienced a decline during the period of the 4.2 ka event, mirroring a general decline in the Jomon culture.

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The 'Repeller of the Amorites' wall was built to defend against nomadic incursions around 2150 BC, potentially linked to societal disruptions from the 4.2 ka event.

Answer: True

Explanation: The 'Repeller of the Amorites' wall, built around 2150 BC, may be linked to societal disruptions and population movements potentially triggered by the aridification and state collapse during the 4.2 ka event.

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The 4.2 ka event is linked to a paleoecological crisis in the Lower Volga region, affecting the Catacomb tribes.

Answer: True

Explanation: A paleoecological crisis during the Middle Bronze Age in the Lower Volga region, linked to the 4.2 ka event, significantly impacted the Catacomb and Post-Catacomb tribes, prompting increased mobility and a shift to nomadic cattle breeding.

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The Liangzhu civilization experienced growth during the 4.2 ka event period.

Answer: False

Explanation: The Liangzhu civilization experienced a decline during the period of the 4.2 ka event, suggesting a potential link between the climatic shift and the civilization's fate.

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Which major ancient civilization's collapse is NOT hypothesized to be linked to the 4.2 ka event?

Answer: Roman Empire

Explanation: While the Old Kingdom of Egypt, Akkadian Empire, and Indus Valley Civilization are hypothesized to have been impacted by the 4.2 ka event, the Roman Empire's collapse occurred much later and is not linked to this specific event.

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The construction of 'motillas' in Spain is proposed as a response to what climatic condition associated with the 4.2 ka event?

Answer: Severe aridification

Explanation: The construction of 'motillas,' ancient groundwater collection systems in La Mancha, Spain, is thought to be a consequence of the severe aridification caused by the 4.2 ka event.

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What evidence from Oman corals suggests a cause for the Akkadian Empire's collapse?

Answer: Prolonged winter 'shamal' seasons causing field salinization.

Explanation: Fossil corals from Oman suggest that prolonged winter 'shamal' seasons around 2200 BC led to field salinization, which reduced crop production and potentially contributed to the Akkadian Empire's collapse.

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According to scholars, what factor besides climate change is believed to have contributed to the Indus Valley Civilization's collapse?

Answer: A decline in trade with Egypt and Mesopotamia.

Explanation: Many scholars believe that drought, coupled with a decline in trade with Egypt and Mesopotamia, contributed to the collapse of the Indus Valley Civilization.

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Which Chinese culture experienced declines potentially linked to the 4.2 ka event?

Answer: Longshan culture

Explanation: The Longshan culture experienced declines potentially linked to the 4.2 ka event, including cooling that reduced rice output, population decrease, and fewer archaeological sites.

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What does reference 61 suggest about the impact on the Catacomb culture in the Lower Volga region?

Answer: It prompted increased mobility and a shift to nomadic cattle breeding due to a paleoecological crisis.

Explanation: Reference 61 suggests that a paleoecological crisis during the Middle Bronze Age in the Lower Volga region affected the Catacomb tribes, prompting increased mobility and a shift to nomadic cattle breeding.

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How did the 4.2 ka event affect the settlement patterns in the Persian Gulf region?

Answer: It caused a sudden change, marking the end of the Umm Al Nar culture and the beginning of the Wadi Suq culture.

Explanation: The 4.2 ka event caused a significant change in the Persian Gulf region, marking the end of the Umm Al Nar culture and the transition to the Wadi Suq culture, with alterations in settlement patterns and pottery styles.

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Scientific Debate and Paleoclimate Proxies

Scientists universally agree that the 4.2 ka event was a global drought with a precisely defined timeline.

Answer: False

Explanation: There is scientific disagreement regarding the characterization of the 4.2 ka event; critics argue that evidence has been conflated and its impact and timing may be more complex and localized than initially proposed.

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The Greenland Gisp2 ice core data shows a prominent signal for the 4.2 ka event, similar to the 8.2-kiloyear event.

Answer: False

Explanation: Unlike the 8.2-kiloyear event, the Greenland Gisp2 ice core data does not exhibit a prominent signal for the 4.2 ka event, suggesting regional differences in its manifestation.

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Jessica Tierney criticizes the Meghalayan age designation because proponents have accurately grouped all evidence.

Answer: False

Explanation: Jessica Tierney criticizes the Meghalayan age designation, arguing that proponents have mistakenly grouped evidence from unrelated periods, rather than accurately compiling it.

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What does the Greenland Gisp2 ice core data indicate regarding the 4.2 ka event?

Answer: It does not show a prominent signal for the event.

Explanation: The Greenland Gisp2 ice core data does not show a prominent signal for the 4.2 ka event, unlike the 8.2-kiloyear event, suggesting regional variations in the event's expression.

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Jessica Tierney's criticism of the Meghalayan age designation centers on which issue?

Answer: Proponents have mistakenly grouped evidence from unrelated periods.

Explanation: Jessica Tierney criticizes the Meghalayan age designation, asserting that proponents have mistakenly grouped evidence from various droughts and wet periods that occurred centuries apart from the actual 4.2 ka event.

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