本研究於中國大陸貴州省雅水剖面晚古生代 Mississippian 晚期 的地層中採取腕足化石，選取 139 個腕足殼體進行研究，並分析 22 個保存良好腕足殼體的碳氧同位素組成及微量元素分析，並進一步討 論在華南地區的碳氧同位素記錄及重建古環境。
保存良好的殼體在碳同位素上，在 Visean 時期，碳同位素平均 值為2.3±2.4‰，在 Serpukhovian 時期，碳同位素平均值為 4.1±2.0‰，
碳同位素值增加 1.8‰，很可能因為有機碳大量埋藏事件有關；而在
氧同位素上，在 Visean 時期，氧同位素平均值為 2.3±2.4‰，在 Serpukhovian 時期，氧同位素平均值為-3.0±0.5 ‰，氧同位素值增加 0.8‰，可能是因為當時冰川體積增加使的氧同位素數值增加。
由於在 Serpukhovian 時期碳氧同位素皆出現突然變輕又變重的 變化，與 Fielding 等人（2008）所研究的冰期，顯示出在 Serpukhovian 時期冰期有間段而不是連續的情形是一致。因此在碳氧同位素同時變 輕為短暫的間冰期。
假設早石炭紀無冰期時，海水的δ18O 數值為-1‰ (SMOW)。上 司階(晚期 Visean)至德塢階(Serpukhovian)平均溫度呈現約下降 3
°C
的現象，與 Mg/Ca 比值所計算之溫度變化大致相同。上司階(晚期 Visean)至德塢階(Serpukhovian)的降溫與碳同位素數值所呈現的碳埋 藏量增加，二氧化碳含量降低的紀錄一致。雅水剖面所呈現之平均值 28°C
至 25°C
的溫暖溫度範圍反映出華南地區於石炭紀位於熱帶地 區海水溫度較高的特性，類似現今西太平洋暖池的溫度特徵。文獻
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