Yes, living things that die in water or near water generally have a higher chance of becoming fossils. There are several reasons for this:
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Rapid Burial: Aquatic environments often have sediment deposition, which can quickly cover organic remains. This rapid burial protects the remains from decomposition and scavenging, allowing conditions suitable for fossilization to occur.
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Anaerobic Conditions: Waterlogged environments often have low oxygen levels, which slows down the decay of organic material. The anaerobic conditions inhibit the activity of bacteria and other organisms that would normally break down dead tissue.
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Sedimentary Processes: Many fossils form in sedimentary rocks, which are commonly associated with water bodies. The geological processes involved in sedimentation favor the preservation of remains found in or near water.
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Preservation of Soft Tissues: In some cases, soft tissues can be preserved in anoxic environments, potentially leading to more detailed fossils, such as those with preserved feathers or skin texture.
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Concentration of Organisms: Aquatic environments can have higher concentrations of organisms, increasing the likelihood that a species will be fossilized over time compared to those living in terrestrial environments, where conditions can be harsher and more variable.
Overall, while fossilization can occur in a variety of environments, the conditions present in and around water bodies tend to be more favorable for the preservation of organic remains.