TOEFL 통합 작문

📖 읽기 지문

The Burgess Shale, a fossil deposit in the Canadian Rockies, has long been celebrated for its exceptional preservation of soft-bodied organisms from the Cambrian period. A prominent interpretation of this fossil assemblage, known as the 'weird wonders' hypothesis, holds that many Burgess Shale animals represent extinct phyla that are fundamentally different from any modern animal groups. Proponents argue that the bizarre morphologies, such as the five-eyed Opabinia and the spiny Hallucigenia, cannot be accommodated within existing taxonomic categories, indicating that the Cambrian explosion produced a greater diversity of body plans than exists today. A second supporting point is that the Burgess Shale fauna exhibit a high degree of morphological disparity, with many species possessing unique features that have no clear counterparts in later fossil records or living organisms. This disparity suggests that many evolutionary experiments were attempted and subsequently abandoned. Finally, the sudden appearance and rapid diversification of these animals in the fossil record, followed by their disappearance in later strata, is interpreted as evidence for mass extinctions that pruned the Cambrian tree of life, eliminating entire lineages that once thrived.

🎧 듣기 강의

The lecture challenges the 'weird wonders' interpretation of the Burgess Shale, arguing that the apparent strangeness of these fossils is largely an artifact of incomplete understanding and biased sampling. First, new analyses using advanced imaging techniques and phylogenetic methods have revealed that many Burgess Shale animals actually possess features that align them with modern phyla. For example, Opabinia, once thought to be unique, is now recognized as an early relative of arthropods, and Hallucigenia has been placed within the onychophoran lineage. Thus, they are not representatives of extinct phyla but rather stem-group members of existing groups. Second, the supposed high disparity may be overestimated because taxonomists have often focused on unusual traits while overlooking shared characteristics. When comprehensive datasets are considered, the range of morphological variation among Burgess Shale animals is comparable to that seen within modern phyla, suggesting that the Cambrian explosion was not an unrivaled burst of innovation. Finally, the disappearance of these animals from later strata does not necessarily indicate mass extinction; it may reflect environmental changes, such as shifts in sedimentation or water chemistry, that reduced fossil preservation potential. Many of these lineages may have continued to evolve into forms we recognize today, leaving no direct fossil evidence due to poor preservation conditions.