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Owing to the time lag, the cumulative effect and the negative feedback between the growth of tree rings and drought stress, the reconstruction of past environment by studying the patterns of tree rings is often inaccurate.
The interpretation of past environment changes in coastal marshes, river mouths and drainage channels connecting fresh to salt water bodies, is a difficult task since several factors must be considered such as the variable influence of climate, sea level changes, coastline variations and changes in the river discharge.
Yet despite growing interest in the drivers of individual differences in information use (Mathot & Dall, 2013), the potential impact of past environment on this trade-off, and hence information gathering via CFL, has not yet been investigated.
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Cave sediments may contain important long-term records of past environments and human activity.
This study provides an isotope-based interpretation of past environments directly linked to the archaeological record.
Therefore, it is necessary to understand the effects of past environments on the distributions of indicator species.
Beetle assemblages also provide highly detailed reconstructions of other aspects of past environments, including vegetation, substrates, and water quality.
Exciting future developments in paleoecology are likely to occur as a result of major advances in Earth sciences and in the reconstruction of past environments from nonbiological evidence.
Few studies, however, have focused on characterizing the entire mineral assemblage, even though it could aide our understanding of past environments.
However, recent studies have suggested the importance of past environments to species distributions (i.e., a time lag between changes in species distribution and habitat alterations).
Because corals are sensitive to changes in light, temperature, water quality, and salinity, their fossils provide information that can be used to interpret climate and geography of past environments.
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