We present the design and synthesis of a small library of substituted biguanidium salts and their capacity to inhibit the growth of pancreatic cancer cells. We first present their in vitro and membrane activity, before we address their mechanism of action in living cells and in vivo activity. We show that phenylethynyl biguanidium salts possess higher ability to cross hydrophobic barriers, improve mitochondrial accumulation and anticancer activity. Mechanistically, the most active compound, 1b, like metformin, activated AMPK, decreased the NAD+/NADH ratio and mitochondrial respiration, but at 800-fold lower concentration. In vivo studies show that compound 1b significantly inhibits the growth of pancreatic cancer xenografts in mice, while biguanides currently in clinical trials had little activity.

We present the design and synthesis of a small library of substituted biguanidium salts and their capacity to inhibit the growth/viability of pancreatic cancer cells. We first present their in vitro and membrane activity, before we address their mechanism of action in living cells and in vivo activity. We show that phenylethynyl biguanidium salts possess higher ability to cross hydrophobic barriers, improved mitochondrial accumulation and anticancer activity. Mechanistically, the most active compound 1b, like metformin, decreases the NAD + /NADH ratio and mitochondrial respiration, but at 800-fold lower concentration. In vivo studies with, the most active, compound 1b show a significant growth inhibition of pancreatic cancer xenografts in mice, while biguanides currently in clinical trials had no activity.

Drilling, 3D seismic and deep seismic studies in recent years have significantly progressed our knowledge of continental margins. Some of the key studies are brought together in this volume, focusing on the evolution and architecture of transform faults and transform margins, giving special attention to the relationship, and differences, between transform and rift margins. Papers from a wide range of global settings consider thermal history, depositional regime, hydrocarbon prospectivity and (in a continental setting) geothermal potential. This scene-setting paper examines our current state of knowledge on transform and rift settings, and provides a brief introduction to the subject matter and context of the papers in the volume.

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