Biomedical subjects

T J Meehan

Publications and source records attributed to T J Meehan.

3 recordsLinked to original sources

PubMed2005

Extinction may not be forever.

Here we review the phenomenon of ecomorph evolution and the hypothesis of iterative climatic cycles. Although a widely known phenomenon, convergent evolution has been underappreciated in both its scope and commonality. The power of natural selection to override genealogy to create similar morphologies (even among distantly related organisms) supports classical Darwinian evolution. That this occurs repeatedly in stratigraphically closely spaced intervals is one of the most striking features of Earth history. Periodic extinctions followed by re-evolution of adaptive types (ecomorphs) are not isolated occurrences but are embedded within complex ecological systems that evolve, become extinct, and repeat themselves in temporal synchrony. These complexes of radiation and extinction bundle the biostratigraphic record and provide the basis for a global stratigraphy. At this scale, climatic change is the only mechanism adequate to explain the observed record of repeating faunas and floras. Understanding of the underlying causes may lead to predictive theories of global biostratigraphy, evolutionary processes, and climatic change.

Animals↗

PubMed2005

Evolution of duplications in the transferrin family of proteins.

The transferrin family is a group of proteins, defined by conserved amino acid motifs and putative function, found in both vertebrates and invertebrates. Included in this group are molecules known to bind iron, including serum transferrin, ovotransferrin, lactotransferrin, and melanotransferrin (MTF). Additional members of this family include inhibitor of carbonic anhydrase (ICA; mammals), major yolk protein (sea urchins), saxiphilin (frog), pacifastin (crayfish), and TTF-1 (algae). Most family members contain two lobes (N and C) of around 340 amino acids, the result of an ancient duplication event. In this article, we review the known functions of these proteins and speculate as to when the different homologs arose. From multiple-sequence alignments and neighbor-joining trees using 71 transferrin family sequences from 51 different species, including several novel sequences found in the Takifugu and Ciona genome databases, we conclude that melanotransferrins are much older (>670 MY) and more pervasive than previously thought, and the serum transferrin/melanotransferrin split may have occurred not long after lobe duplication. All subsequent duplication events diverged from the serum transferrin gene. The creation of such a large multiple-sequence alignment provides important information and could, in the future, highlight the role of specific residues in protein function.

Amino Acid Sequence↗

PubMed2003

Extinction and re-evolution of similar adaptive types (ecomorphs) in Cenozoic North American ungulates and carnivores reflect van der Hammen's cycles.

Numerous patterns in periodicity (e.g., climate, extinction, and sedimentary cycles) and evolutionary change (e.g., chronofaunas and coordinated stasis) have been described based on aspects of the geologic record. Recently, convergent occurrences of faunal types or "repeating faunas" have received attention, but a highly specific, iterative pattern was first reported over 40 years ago. In the late 1950s, van der Hammen described climatic/floral cycles on the order of six million years based on a succession of A, B, and C pollen community types in South America. These A-B-C cycles are also seen in the replacement pattern of particular carnivore and ungulate adaptive types in Cenozoic North America as reported by Martin in the 1980s. For example, in the last 36 million years, there were four iterations of a sabertooth cat ecomorph independently evolving, dominating the niche through an A-B-C cycle, and then going extinct. Here we show further support for the existence of these cycles in the dominance turnover in hippo and dog ecomorphs in the North American Cenozoic. Shared patterns of extinction and re-evolution of adaptive types among plants and mammals across two continents suggest a global mechanism, which appears to be climatic change. Iterative climatic cycles of various scales may form a predictive framework for understanding fundamental patterns in the geologic record, such as radiations, extinction, rates of change, convergence, and sedimentary cycles.

Acclimatization↗