The global transcriptional coactivators CREB-binding protein (CBP) and the closely related p300 interact with over 312 proteins, making them among the most heavily connected hubs in the known mammalian protein-protein interactome. It is largely uncertain, however, if these interactions are important in specific cell lineages of adult animals, as homozygous null mutations in either CBP or p300 result in early embryonic lethality in mice. Here we describe a Cre/LoxP conditional p300 null allele (p300 flox ) that allows for the temporal and tissue-specific inactivation of p300. We used mice carrying p300 flox and a CBP conditional knockout allele (CBP flox ) in conjunction with an Lck-Cre transgene to delete CBP and p300 starting at the CD4 ؊ CD8 ؊ double-negative thymocyte stage of T-cell development. Loss of either p300 or CBP led to a decrease in CD4 ؉ CD8 ؉ double-positive thymocytes, but an increase in the percentage of CD8 ؉ single-positive thymocytes seen in CBP mutant mice was not observed in p300 mutants. T cells completely lacking both CBP and p300 did not develop normally and were nonexistent or very rare in the periphery, however. T cells lacking CBP or p300 had reduced tumor necrosis factor alpha gene expression in response to phorbol ester and ionophore, while signal-responsive gene expression in CBP-or p300-deficient macrophages was largely intact. Thus, CBP and p300 each supply a surprising degree of redundant coactivation capacity in T cells and macrophages, although each gene has also unique properties in thymocyte development.

The C-terminal activation domain (C-TAD) of the hypoxiainducible transcription factors HIF-1a and HIF-2a binds the CH1 domains of the related transcriptional coactivators CREB-binding protein (CBP) and p300, an oxygen-regulated interaction thought to be highly essential for hypoxiaresponsive transcription. The role of the CH1 domain in vivo is unknown, however. We created mutant mice bearing deletions in the CH1 domains (DCH1) of CBP and p300 that abrogate their interactions with the C-TAD, revealing that the CH1 domains of CBP and p300 are genetically non-redundant and indispensable for C-TAD transactivation function. Surprisingly, the CH1 domain was only required for an average of B35-50% of global HIF-1-responsive gene expression, whereas another HIF transactivation mechanism that is sensitive to the histone deacetylase inhibitor trichostatin A (TSA S ) accounts for B70%. Both pathways are required for greater than 90% of the response for some target genes. Our findings suggest that a novel functional interaction between the protein acetylases CBP and p300, and deacetylases, is essential for nearly all HIF-responsive transcription.

Halite crystals were selected from a 186 m subsurface core taken from the Badwater salt pan, Death Valley, California to ascertain if halophilic Archaea and their associated 16S rDNA can survive over several tens of thousands of years. Using a combined microscope microdrill/micropipette system, fluids from brine inclusions were aseptically extracted from primary, hopper texture, halite crystals from 8 and 85 metres below the surface (mbls). U-Th disequilibrium dating indicates that these halite layers were deposited at 9,600 and 97,000 years before present (ybp) respectively. Extracted inclusions were used for polymerase chain reaction (PCR) analysis with haloarchaea-specific 16S rDNA primers or placed into haloarchaea culture medium. Enrichment cultures were obtained from 97 kyr halite crystal inclusion fluid and haloarchaea-containing prepared crystals (positive controls), whereas inclusions from crystals of 9.6 kyr halite and the haloarchaea-free halite crystals (negative controls) resulted in no growth. Phylogenetic analysis (16S rDNA) of the 97 kyr isolate, designated BBH 001, revealed a homology of 100% with Halobacterium salinarum. DNA-DNA hybridization experiments confirmed that BBH 001 was closely related to H. salinarum (81-75% hybridization) and its ascription to this haloarchaea species. The described method of retrieving particle-containing brine from fluid inclusions offers a robust approach for assessing the antiquity of microorganisms associated with evaporites.