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Student analysis of the last 1000 years of the Gulf of Mexico hypoxia zone (informally "dead" zone) by using relative abundance of low-oxygen tolerant benthic foraminifera. In this example of environmental micropaleontology, students evaluate whether the "dead" zone has existed in its current form for many centuries or has become more intense in the time of increased anthropogenic input of organics (i.e., fertilizer).
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