Question: Were the two documentaries, Iran and The Last Days of Left Eye, both made more than 10 years ago?

<P0-S0> The Last Days of Left Eye is a documentary directed by Lauren Lazin which premiered on VH1 and VH1 Soul on May 19, 2007. <P0-S1>  Filmed from March 30, 2002 until her death on April 25, 2002, it centered on the life, last days spent in spiritual retreat in Honduras, and accidental death of rapper and TLC member Lisa Lopes (May 27, 1971 — April 25, 2002), featuring narrative insight and commentary from interviews of the singer. <SEP> <P1-S0> Iran (is not the problem) or Iran is not the problem (2008) Iranian documentary film directed, produced and written by Aaron Newman. <SEP> <P2-S0> Lauren Lazin is an American filmmaker whose first feature film, "" was nominated for a 2005 Academy Award. <P2-S1>  Her follow-up film, "I'm Still Here: Real Diaries of Young People Who Lived During the Holocaust" was nominated for two 2006 Emmy Awards, and was named Best Documentary by the National Foundation for Jewish Culture. <P2-S2>  She was also the director of the documentary "The Last Days of Left Eye" which looked at the life and death of Lisa "Left Eye" Lopes of TLC. <SEP> <P3-S0> Before photosynthesis evolved, Earth's atmosphere had no free oxygen (O). <P3-S1>  Photosynthetic prokaryotic organisms that produced O as a waste product lived long before the first build-up of free oxygen in the atmosphere, perhaps as early as 3.5 billion years ago. <P3-S2>  The oxygen they produced would have been rapidly removed from the atmosphere by weathering of reducing minerals, most notably iron. <P3-S3>  This "mass rusting" led to the deposition of iron oxide on the ocean floor, forming banded iron formations. <P3-S4>  Oxygen only began to persist in the atmosphere in small quantities about 50 million years before the start of the Great Oxygenation Event. <P3-S5>  This mass oxygenation of the atmosphere resulted in rapid buildup of free oxygen. <P3-S6>  At current rates of primary production, today's concentration of oxygen could be produced by photosynthetic organisms in 2,000 years. <P3-S7>  In the absence of plants, the rate of oxygen production by photosynthesis was slower in the Precambrian, and the concentrations of O attained were less than 10% of today's and probably fluctuated greatly; oxygen may even have disappeared from the atmosphere again around 1.9 billion years ago. <P3-S8>  These fluctuations in oxygen concentration had little direct effect on life, with mass extinctions not observed until the appearance of complex life around the start of the Cambrian period,   million years ago . <P3-S9>  The presence of O2 provided life with new opportunities. <P3-S10>  Aerobic metabolism is more efficient than anaerobic pathways, and the presence of oxygen undoubtedly created new possibilities for life to explore. <P3-S11>  Since the start of the Cambrian period, atmospheric oxygen concentrations have fluctuated between 15% and 35% of atmospheric volume. <P3-S12>  The maximum of 35% was reached towards the end of the Carboniferous period (about 300 million years ago), a peak which may have contributed to the large size of insects and amphibians at that time. <P3-S13>  Whilst human activities, such as the burning of fossil fuels, affect relative carbon dioxide concentrations, their effect on the much larger concentration of oxygen is less significant.