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The role of protoplanetary disks in rocky planet formation

Protoplanetary disks around young stars of less than 10 million years old are the birth cradles of planets. Observations with ALMA have provided us with a wealth of data on the gas and dust distribution in protoplanetary disks and the early signs of planet formation. Whereas gaps in disks provide evidence for the rapid formation of gas giants, rocky planet formation remains more challenging to observe directly at this stage. On the other hand, several new insights have been obtained in the context of dust evolution in disks, such as coagulation, fragmentation and transport of dust pebbles in the first few million years of the lifetime of the disk. In this talk I will present an overview of our current knowledge of protoplanetary disks and their potential of forming rocky planets.

2 February 2023

13:00 UTC

Considering chemical evolution toward life on Earth from Enceladus

Saturn's moon Enceladus possesses a Na-carbonate-rich subsurface ocean. According to the in-situ analysis of plume materials erupting from the subsurface ocean, the Cassini spacecraft has revealed that seawater pH is alkaline, near 10, and that hydrothermal activity exists in the rock core. In addition to Na-carbonate-rich plume particles, a new type of phosphate-rich particle was recently discovered. Phosphorus (P) is a CHNOPS element essential for life on Earth, but of these, it is the least abundant in the Earth's aqueous environments. Throughout Earth's history, phosphorus has been the rate-limiting element of biological production. Based on the analysis of phosphate-rich particles of Enceladus, phosphate concentrations in the subsurface ocean would be 1000 times higher than in the Earth's oceans.

To understand the causative mechanism of the enrichment of phosphate in Enceladus' seawater, we performed hydrothermal reaction experiments and geochemical modeling. We find that alkaline (pH ~10) and carbonate-rich aqueous environments are essential for the phosphate enrichment, where calcium phosphate minerals are thermodynamically unstable compared to calcium carbonate minerals, releasing phosphate into liquid phase. Such alkaline carbonate-rich aqueous environments are commonly achieved in icy ocean worlds beyond the CO2 snowline of the Solar System. Phosphate could have been also enriched in similar alkaline carbonate-rich aqueous environments on early Earth, where earliest life on Earth might have utilized phosphorus as components of its building materials.

Detecting and Characterizing Terrestrial Exoplanets: Earth-like planets, their atmospheres and habitability


Past Meetings

1 December 2022

15:00 UTC

Volatile accretion and evolution in the terrestrial planets

Planetary habitability is tied to the history of volatile accretion, volatile loss, and the evolution of surficial environments. Habitability is particularly related to the record of the life essential volatile elements such as hydrogen, carbon, nitrogen and sulfur. Noble gases are another set of volatile elements, but given their inert nature, are neither relevant for pre-biotic chemistry, or for life itself. And yet, the noble gases are intricately linked to the question associated with the planetary habitability and the origin of life through the remarkable portrait that they paint of the processes associated with the formation and evolution of a habitable planet. For example, the noble gas isotopes record processes associated with volatile delivery, how volatile sources changed through time, volatile loss, the evolution of the early atmosphere, and volatile exchange between the surface and the interior of a planet. It is this process-based framework provided by the noble gases that can be utilized as constraints towards constructing models around planetary habitability. An especially powerful approach is to integrate noble gas observations and models with those from hydrogen, carbon, nitrogen and sulfur. In this presentation, I will discuss how to read the noble gas record, recent work that is shaping our understanding of the volatiles in the inner Solar System, and where the frontiers and challenges lie in building a generalized framework for understanding volatile evolution in rocky planets.

3 November 2022

13:00 UTC

Impact-driven atmospheric loss from terrestrial planets

Determining how terrestrial planets accrete and retain volatile elements is fundamental for understanding planetary diversity, evolution, and habitability. One mechanism that could play an important role in determining planetary volatile budgets is the loss of existing atmospheres (and potentially oceans) driven by impacts. I will demonstrate how the pre-impact surface conditions and distribution of volatiles on colliding bodies can dictate the efficiency by which different volatiles are lost in impact events. In particular, I will show that planets that experience more giant impacts later in accretion are much more suspectable to atmospheric loss.

An Interdisciplinary (Preliminary) Understanding of Planetary Evolution

The key to finding life on an exoplanet lies within the atmospheres of extrasolar planets, which have just recently become accessible to chemical analysis. The only way to detect a true ‘biosignature’—a definitive marker for life—is to rule out all abiotic processes that could lead to a ‘false positive.’ Thick atmospheres enshroud the interiors of the most common types of rocky planets. These planets’ geologic evolution is inextricably tied to their atmospheres in ways we don’t yet fully understand. To reveal the intricacies of this connection and ultimately open the door to the reliable detection of life beyond Earth we need a diverse team, access to facilities, and resources that will catalyze new discoveries and advance a new scientific paradigm. To accurately use planetary atmospheres as a proxy for life, establishing a baseline for a planet is critical. Atmospheres are complex, both physically and chemically. They are modified not only by the stellar insolation they receive from above but by the rocky surface below. The interiors and atmospheres of rocky planets interact initially during the magma ocean stage, that could last for a billion years, and then more slowly due to weathering, volcanism, and subduction. Our AEThER team has begun a coordinated scientific effort employing experimental, theoretical, and empirical approaches to address challenging yet fundamental questions, including: What is the principal control on planetary atmospheres from accretion until the time life begins to modify the signal? How sensitive is atmospheric chemistry to interior chemistry? This talk will discuss our current findings as well as our future directions.