Exact(16)
Map overlaying allowed analyzing the time depth and landscape constancy.
The time depth of the Qesem Cave and its deposits also makes these findings groundbreaking.
Since we know that the time depth of divergence among these Burmic languages is probably less than two millennia, this illustrates how substantially the system of an individual language can change.
However, a more nuanced approach in terms of looking at the time depth in the archaeological record is to examine how differential attributes behave over time to identify them as either stylistic or functional.
Although, due to the time depth that natural selection can take into account, it seems ideal for addressing questions about the material culture that represents human behavior in the archaeological record, we must somehow use the present without biasing our view of the past.
Although there is little consideration of tenure systems and aspects of worldviews and social relations in these early ethnographic sources, there are nuggets of information about management and tenure that reflect the time depth of these practices (e.g., Drucker 1951; Stern 1934).
Similar(44)
Computational methods for calculating the "time depths" of language families have been proposed, but they have not been shown to yield reliable results.
It may also reflect stochastic variance in the time depths of the coalescent of the ancestral population into which the lineages from the extant species descend.
It also facilitates a landscape approach to archaeology, enabling sites to be appreciated within their wider geographical and archaeological context and demonstrating the time-depth of that landscape.
This grouping process is defined through a similarity measure of neighboring segments, which is based on intensity, speed and the time-depth of motion-history.
Here we present sedimentological and petrographical data to elucidate the depositional environment and sedimentary processes responsible for hydrothermal carbonate precipitation and early diagenetic alteration as well as clastic sediment accumulation and provide initial 230Th/U ages to constrain the time-depth of this travertine colluvium succession.
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Justyna Jupowicz-Kozak
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