That's because the animal doesn't have much protection until it develops its shell and becomes an adult, and acidic conditions could interfere
with shell formation (ie - calcification).
Not exact matches
In 1968, two researchers from Fort Hays Kansas State College studying cephalopods from the Niobrara
Formation compared the specimen
with a cuttlefish, based primarily on its textural similarities to a cuttlebone — the unique internal
shell of cuttlefish.
While on present - day Earth the carbonate
formation is dominantly through organic processes (various
shell - forming marine organisms are happy to make use of the CO2 dissolved in the ocean), in the early Earth and, presumably, in other Earth - like planets
with little or no life the same process can occur inorganically, but somewhat slower, in silicate rock weathering.
«When CO2 reacts
with seawater, the reduction in seawater pH reduces the availability of carbonate ions, which play an important role in
shell formation for a number of marine organisms such as corals, marine plankton, and shellfish.