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Chappell, G.

Publications and source records attributed to Chappell, G..

2 recordsLinked to original sources

CCDC32 collaborates with the membrane to assemble the AP-2 clathrin adaptor complex

Cells have evolved a variety of assembly chaperones to aid in the difficult process of forming macromolecular complexes in a crowded cytoplasm. Assembly of adaptor protein complex 2 (AP-2), the primary cargo adaptor in clathrin-mediated endocytosis, is regulated by the chaperones AAGAB and CCDC32, whose deletion causes loss of all AP-2 subunits in vivo. AAGAB and CCDC32 are thought to act sequentially to assemble the AP-2 tetramer from its constituent heterodimers. However, the molecular requirements and structural consequences of CCDC32 interaction with AP-2 are not yet understood. Here, using in vitro reconstitution and integrative structural analysis, we describe the molecular mechanism of CCDC32-mediated AP-2 assembly. First, CCDC32 interacts with the appendage domain of the AP-2 subunit, using the same binding site as canonical endocytic regulators in addition to a novel, yet highly conserved pocket on . CCDC32 contains cargo sorting motifs normally found in trans-membrane cargo and binds to AP-2 heterodimers using canonical cargo-binding sites. Additionally, two amphipathic helices in CCDC32 bind to the /{sigma}2 heterodimer. Surprisingly, in solution, we find that CCDC32 prevents complex assembly and actively disassembles AP-2 tetramers. Inhibition requires the amphipathic helices of CCDC32, which also mediate binding to PIP2-containing membranes. The presence of PIP2-containing membrane stabilizes the final stages of assembly. We propose that the membrane acts as a molecular switch to release inhibitory interactions, allowing for full complex assembly to proceed. Using cryo-EM, we visualize an assembly intermediate that mimics the conformation of AP-2 found in vesicles, with CCDC32 bound at both cargo binding sites and both membrane-binding sites, suggesting that assembly leads to deposition of active complexes on the plasma membrane.

molecular biology↗

The evolution and spread of sulfur-cycling enzymes reflect volcanic sulfur sources and the redox state of the early Earth

The biogeochemical sulfur cycle plays a central role in fueling microbial metabolisms, regulating the Earths redox state, and impacting climate. However, geochemical reconstructions of the ancient sulfur cycle are confounded by ambiguous isotopic signals. Here, we use phylogenetic reconciliation to ascertain the timing of ancient sulfur cycling gene events across the tree of life. Our results suggest that metabolisms using sulfide oxidation emerged in the Archean, but those involving thiosulfate emerged only after the Great Oxidation Event. Our data reveal that observed geochemical signatures resulted not from the expansion of a single type of organism, but were instead associated with genomic innovation across the biosphere. Moreover, our results provide the first indication of organic sulfur cycling from the mid-Proterozoic onwards, with implications for climate regulation and atmospheric biosignatures. Overall, our results provide insights into how the biological sulfur cycle evolved in tandem with the redox state of the early Earth. Teaser: Phylogenomics analyses reveal that the evolution of microbial sulfur metabolisms co-evolved with the redox state of the early Earth.

evolutionary biology↗