the hypsithermal interval occurred approximately 8,000 years ago.
間冰期大約發生在8000年前。
during the hypsithermal period, global temperatures peaked.
在間冰期期間，全球溫度達到峰值。
scientists study the hypsithermal epoch to understand past climates.
科學家研究間冰期來了解過去的氣候。
the hypsithermal climate supported diverse forest ecosystems.
間冰期的氣候支持了多樣的森林生態系統。
archaeological evidence reveals hypsithermal conditions in this region.
考古證據顯示此地區存在間冰期的條件。
the hypsithermal maximum occurred during the holocene.
間冰期的最高溫度發生在全新世。
early hypsithermal warming led to significant ecological changes.
早期間冰期的暖化導致了顯著的生態變化。
late hypsithermal vegetation patterns differed from earlier periods.
晚期間冰期的植被模式與早期時期不同。
the hypsithermal onset marked a major climatic transition.
間冰期的開始標誌著一次重要的氣候轉變。
researchers analyze hypsithermal proxy data from lake sediments.
研究人員分析來自湖床沉積物的間冰期代理數據。
paleoclimatic records indicate an extended hypsithermal phase.
古氣候記錄顯示間冰期階段持續較長時間。
the hypsithermal interval occurred approximately 8,000 years ago.
間冰期大約發生在8000年前。
during the hypsithermal period, global temperatures peaked.
在間冰期期間，全球溫度達到峰值。
scientists study the hypsithermal epoch to understand past climates.
科學家研究間冰期來了解過去的氣候。
the hypsithermal climate supported diverse forest ecosystems.
間冰期的氣候支持了多樣的森林生態系統。
archaeological evidence reveals hypsithermal conditions in this region.
考古證據顯示此地區存在間冰期的條件。
the hypsithermal maximum occurred during the holocene.
間冰期的最高溫度發生在全新世。
early hypsithermal warming led to significant ecological changes.
早期間冰期的暖化導致了顯著的生態變化。
late hypsithermal vegetation patterns differed from earlier periods.
晚期間冰期的植被模式與早期時期不同。
the hypsithermal onset marked a major climatic transition.
間冰期的開始標誌著一次重要的氣候轉變。
researchers analyze hypsithermal proxy data from lake sediments.
研究人員分析來自湖床沉積物的間冰期代理數據。
paleoclimatic records indicate an extended hypsithermal phase.
古氣候記錄顯示間冰期階段持續較長時間。
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