Needle-fiber calcite (NFC)
is common diagenetic cement that has been found globally in many different
types of limestone. The origin of NFC has been widely debated, and both
abiogenic and biogenic processes have been invoked to explain its origin. In
recent years, the origin of NFC has been closely allied to fungi. Jones and Peng document NFC in the spring
deposit at Shiqiang, Yunnan Province, China, where NFC is common—but never associated
with fungi. The study explores the different possible mechanisms and concludes
that these NFC formed by abiogenic processes, driven largely by evaporation. These
results highlight the critical problems in trying to ascertain the origin of
carbonate cements, and the dangers of trying to ascribe all NFC to biogenic
processes.
Abiogenic growth of needle-fiber calcite in spring towers at Shiqiang, Yunnan Province, China by Brian
Jones and Xiaotong Peng
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