Complex organics in space from Solar System to distant galaxies

Recent observational and experimental evidence for the presence of complex organics in space is reviewed. Remote astronomical observations have detected ∼\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\sim $$\end{document}200 gas-phased molecules through their rotational and vibrational transitions. Many classes of organic molecules are represented in this list, including some precursors to biological molecules. A number of unidentified spectral phenomena observed in the interstellar medium are likely to have originated from complex organics. The observations of these features in distant galaxies suggests that organic synthesis had already taken place during the early epochs of the Universe. In the Solar System, almost all biologically relevant molecules can be found in the soluble component of carbonaceous meteorites. Complex organics of mixed aromatic and aliphatic structures are present in the insoluble component of meteorites. Hydrocarbons cover much of the surface of the planetary satellite Titan and complex organics are found in comets and interplanetary dust particles. The possibility that the early Solar System, or even the early Earth, have been enriched by interstellar organics is discussed.


Introduction
Before the nineteenth century, organic matter was assumed to be associated only with life and was believed to possess a special quality called the "vital force". This belief was based on the fact that biologically related molecules were all derived from B Sun Kwok sunkwok@hku.hk living organisms. For example, the amino acid asparagine was derived from asparagus, leucine from cheese, glycine from gelatin, and living yeast was needed for fermentation of sugar into alcohol. However, advances in laboratory chemical techniques have made possible the artificial synthesis of urea (CO(NH 2 ) 2 ) from ammonium cyanate (NH 4 CNO) in 1823, amino acid alanine from acetaldehyde, ammonia, and hydrogen cyanide in 1850, and sugars from formaldehyde in 1861. The ability to synthesize organic matter from inorganic ingredients has led to the demise of the "vital force" concept. We now define organics as the class of molecules and compounds based on the element carbon, but they contain also other elements such as H, O, N, S, and P.
On Earth, organic matter as the result of life is present in the oceans, in the atmosphere, and on the Earth's crust. However, the total amount of biomass (∼2000 giga tons) pales in comparison to the amount of kerogen, (>1.5 × 10 7 giga tons), a complex, high molecular weight organic matter found in sedimentary rocks (Falkowski et al. 2000). Kerogen is believed to be a precursor of fossil fuels such as oil, coal, and natural gas and therefore represents remnants of past life on Earth (Dow 1977).
Until very recently, complex organics was thought to be in the exclusive domain of the Earth. The detection of a large number of gas-phase organic molecules in the interstellar medium through their rotational and vibrational transitions gave us the first hint that organic matter can be naturally synthesized in space. Solid-state particles (commonly referred to in the astronomical literature as dust or grains) have been known to exist in the interstellar medium through the technique of selective extinction for about 100 years. Early suggestions of the chemical structure of interstellar solids included graphite, iron, and ice. The detection of the 10 µm silicate feature in evolved stars and in the interstellar medium in the late 1960s led to the realization that minerals such as amorphous silicates are a major component of interstellar solids (Woolf and Ney 1969). Although the existence of organic solids in space has been speculated for some time (Hoyle and Wickramasinghe 1977;Knacke 1977), this idea has never been taken seriously by the astronomical community until recently. There is now strong evidence that complex organic matter is widely present in the Solar System, in the circumstellar environment of stars, in interstellar clouds, in the diffuse interstellar medium, and in distant galaxies. In this paper, I will review our current observational evidence for complex organics in various astronomical environments and discuss the chemical structure and origins of organic solids in space.

Organic molecules in the gas phase
The first interstellar molecules detected were CN, CH, and CH + through their electronic transition in absorption against background starlight (McKellar 1940). The possibility of detecting molecular transitions in the microwave part of the electromagnetic spectrum was recognized by Shklovsky and Townes in the early 1950s (Townes 1957). In spite of this knowledge, the general feeling in the astronomical community was that it is unlikely for molecules other than simple radicals to exist in space because of the low gas density and high ultraviolet radiation background (see, e.g., Townes 2006). Search for molecular transitions was made possible by technical advances in microwave, millimeter-wave and infrared detectors in the 1960s.
Large asymmetric organic molecules have complicated energy structures and correspondingly large partition functions. Their populations are spread over many energy states, making individual rotational transitions weak (Kwok 2006). A firm detection of complex gas-phase organic molecules requires the matching of multiple transitions. Some simple asymmetric molecules such as methanol (CH 3 OH), and to a less extent dimethyl ether (CH 3 OCH 3 ), vinyl cyanide (CH 2 CHCN), ethanol (C 2 H 5 OH), and methyl formate (HCOOCH 3 ), are so abundant and have so many transitions that their lines crowd out the weaker lines of more complex molecules. The sensitivities of modern millimeter (mm) and submm-wave telescopes are so high and the quantity of interstellar molecules so abundant that practically every spectral region of the mm/submm spectrum is filled with some molecular line. This is evident in spectral line surveys carried out by modern telescopes such as the Herschel Space Telescope Crockett et al. 2014). This phenomenon, known as line confusion, greatly limits our ability to search for weaker lines. The failure to detect complex organic molecules through their rotational transitions therefore does not necessarily imply the absence or low abundance of the molecules.
The classes of carbohydrates, lipids, proteins, and nucleic acids form the four basic classes of organic molecules of life. One of the major recent efforts in astrochemistry has been to search for the building blocks of these molecules. In this review, we will concentrate on the study of complex organics. A review of simpler gas-phase organic molecules, in particular those in dense molecular clouds, can be found in Caselli and Ceccarelli (2012). Below, we will summarize some of the progress made in the search for complex organics in the Universe.

Amines and amides
The element nitrogen (N) plays an important role in biochemistry as it is needed in the synthesis of amino acids and nucleotides. Hydrogen cyanide (HCN), a precursor of many biomolecules, and the family of cyanopolynnes (HC n N) are easily detectable through their rotational transitions because of the linear structure of the molecules and their degenerate rotational states. The wide presence of N-containing molecules in the interstellar medium provides the confidence needed that the N is indeed available for biochemical synthesis in space.
Urea ((H 2 N) 2 CO) was the first biomolecule synthesized in the laboratory, demonstrating the ingredients of life can be artificially manufactured. The detection of urea in space would therefore possess special significance. Although the rotational spectra of urea is well known, the spectral complexity of the molecules makes definite detection of this molecule difficult (Remijan et al. 2014).

Amino acids and proteins
There have been extensive searches for glycine, the simplest amino acid (Kuan et al. 2003a, b;Snyder et al. 2005), but so far there has been no concrete evidence for its detection Jones et al. 2007). Glycine in the interstellar medium is assumed to be formed on ice under UV irradiation (Kim and Kaiser 2011). The immediate precursors of gylcine are CH 3 NH 2 (formed with CO 2 ) or CH 2 NH 2 (formed with HCN), both of which have been detected (Kaifu et al. 1974;Ohishi 2015). Amino acetonitrile (NH 2 CH 2 CN), a molecule chemically related to glycine although not necessarily its precursor, has also been detected (Belloche et al. 2008).

Heterocyclic molecules
Planar rings with N, O, or S replacing one of the C atoms on the ring are important building blocks of biomolecules. Examples of precursors to heterocyclic molecules include furan (C 4 H 4 O), pyrrole (C 4 H 5 N), and imidazole (C 3 H 4 N 2 ). Pyrrole serves as a precursor for the side train of the amino acid proline and is a constituent of the heme groups in hemoglobin and chlorophyll. Imidazole is formed as a side chain in the amino acid histidine and the biomolecule histamine. The monocyclic pyrimidine (c-C 4 H 4 N 2 ) and bicyclic purine (c-C 5 H 4 N 4 ) molecules are the parents of the nucleobases. Pyrimidine is the base for cytosine (DNA and RNA), thymine (DNA), and uracil (RNA), whereas purine is the basis for adenine and guanine (in both DNA and RNA).
The structures of these molecules are simple enough that it is possible to search for them via their rotational transitions. However, searches to date have yielded only negative results [pyrrole: Kutner et al. (1980), furan: Dickens et al. (2001), imidazole: Irvine et al. (1981), pyrimidine: Charnley et al. (2005)].

Organics in the Solar System
While astronomical sources are only accessible by remote passive observations, Solar System objects have the advantage that physical samples can be measured or analyzed directly. Meteorites are extraterrestrial objects that can be retrieved from the surfaces of the Earth. Interplanetary dust particles can be collected from the upper atmosphere by high-flying aircrafts. Space probes have been sent to asteroids, comets and planetary satellites to measure their chemical compositions in situ. Samples have been retrieved from the Moon, asteroids, and comets and returned to earth for analysis.
Techniques used to analyze samples can be passive and non-destructive, e.g., through imaging and spectroscopy. Examples include nuclear magnetic resonance (NMR), fourier transform infrared spectroscopy (FTIR), X-ray absorption near edge spectroscopy (XANES), electron paramagnetic resonance (EPR), high resolution transmission electron microscopy (HRTEM). Alternatively, the samples can be altered by heating or dissolving in a solvent. The technique of pyrolysis gas chromatography heats a sample to release smaller molecules that can be separated and identified. The technique of secondary ion mass spectroscopy (SIMS) uses a beam of ions to sputter layers of sample and subject them to mass analysis.

Meteorites
When complex organics was first discovered in meteorites (Nagy et al. 1961), it took the scientific community by surprise. In the 50 years since, we have learned that almost all biologically relevant organic compounds have been found to be present in carbonaceous meteorites. In the soluble component of meteorites, over 14,000 compounds with millions of diverse structures have been identified. These include carboxylic acids, sulfonic and phosphonic acids, amino acids, aromatic hydrocarbons, heterocyclic compounds, aliphatic hydrocarbons, amines and amides, alcohols, aldehydes, ketones, and sugar related compounds (Schmitt-Kopplin et al. 2010). The decreasing abundance with increasing carbon number within the same class of compounds suggests that they are of abiotic origin.
Included in the soluble component of meteorites are over 100 amino acids (Pizzarello and Shock 2010), far more than the 20 present in proteins in biological organisms on Earth. Amino acids with both D (right-handed) and L (left-handed) chirality are represented in meteorites. This is clearly distinct from terrestrial amino acids where only L chirality is present in biological proteins (Pizzarello and Cronin 2000). The slight excess of L-amino acids observed in meteorites, if delivered to the Early Earth and amplified, may be responsible for the homochirality in terrestrial life (Aponte et al. 2014). The discovery of terrestrially rare nucleobases 2,6-diaminopurine and 6,8-diaminopurine in the meteorites suggests that there is a broader range of biochemistry possible in the Universe (Callahan et al. 2011).
Over 70 % of the organics in carbonaceous chondrites are in the form of insoluble organic matter (IOM). The chemical structure of these insoluble macromolecular solids consists of small (1-4) aromatic rings, short aliphatic chains, and contain hetero elements such as O, S, and N (Derenne and Robert 2010;Cody et al. 2011). These structures are very similar to those of terrestrial kerogen and coal (Kerridge 1999;Sephton et al. 2004). In terms of abundance, the ratios of the atoms can be expressed as C 100 H 46 N 10 O 15 S 4.5 (Pizzarello and Shock 2010).
The extensive varieties of organics in meteorites is evidence that abiotic synthesis of complex organics is possible in the extraterrestrial environment. What is not clear is whether these organics were made in the Solar System, or they were inherited from the interstellar medium. The excesses in D and 13 C abundance relative to the solar value are possible indicators of their interstellar origin.
Since comets are sources of meteorites and interplanetary dust particles (IDPs), the organics similar to IOM are expected to be present in comets as well. Complex hydrocarbons are found in the samples returned by the Stardust mission to the Comet 81P/Wild 2 (Keller et al. 2006;Clemett et al. 2010). Figure 1 shows the 3.3 µm aromatic and 3.4 µm C-H stretching mode features observed in this comet are very similar to the unidentified infrared emission (UIE) bands found in the interstellar medium (Sect. 4.3). Some particles in the Stardust sample have been identified to be of interstellar origin (Westphal 2014). A broad 2.9-3.6 µm feature detected by the Visible InfraRed and Thermal Imaging Spectrometer (VIRTIS)on Rosetta is attributed to nonvolatile organic macromolecular materials on the nucleus of comet 67P/Churyumov-Gerasimenko (Capaccioni et al. 2015).
Among the biomolecules detected in the Stardust sample is glycine. Carbon isotopic ratios of the molecule suggests that it is of clear extraterrestrial origin (Elsila et al. 2009).

Asteroids
Some asteroids have very red colors and low (0.01-0.15) albedos which are inconsistent with a mineral or ice composition. These properties are more compatible with complex organics, as macromolecular carbon compounds tend to have dark red, brown, or black colors (Gradie and Veverka 1980). Tholins, an artificial amorphous substance produced by UV photolysis of gas mixtures of N 2 , NH 3 , and CH 4 (Sagan and Khare 1979), has been suggested as one of such possible organic constitutes of asteroids (Cruikshank and Imanaka 2005). The detections of the 3.4 µm feature in the asteroids 24 Themis and 65 Cybele support the presence of complex organics on the surface of these asteroids (Campins et al. 2010;Licandro et al. 2011).
Samples returned from the near-Earth S-type asteroid Itokawa by the Hayabusa mission have been found to consist of mostly silicate minerals without any detectable amount of organics (Naraoka et al. 2015).

Interplanetary dust particles
Interplanetary dust particles (IDP) are micron-size fragments of comets and asteroids. IDPs are often carbon rich (up to 50 % in weight), highly porous, and have not been significantly aqueously altered. As the Earth orbits the Sun, IDPs are swept up by the moving Earth and every year 20,000 to 60,000 tons of IDPs enter the Earth's atmosphere. These particles can be collected by high-flying aircraft and brought back to the laboratory for analysis. The chemical structures of IDPs can be determined by infrared spectroscopy, Raman spectroscopy, microprobe laser desorption mass spectrometry (μL 2 MS), and X-ray absorption near-edge structure spectroscopy (XANES). Complex aromatic compounds were first detected by μL 2 MS (Clemett et al. 1993). Infrared spectroscopy of IDPs shows aromatic and aliphatic 3.3 and 3.4 µm features (Matrajt et al. 2013) (Fig. 2). Evidence of carbonate, oxygen, and nitrogen function groups can be found by XANES .
The large isotopic fractionation in the organic matter in IDPs (D/H and 15 N/ 14 N) has been considered by some to represent preserved interstellar organic material (Messenger and Nakamura -Messenger 2015).
Micrometeorites are similar to IDP except in the collection method. Particles collected in icefields of Antarctica and Greenland are called micrometeorties, in contrast to IDPs which are collected in the upper atmosphere. For example, micrometeorties have been collected in Dome Fuji and Dome C in Antarctica by Japanese and French/Italian teams respectively. Analysis of the organic content of Antarctic micrometeorites shows excess amount of N over the typical N to C ratios observed in IOM. Since there is not yet any evidence for the existence of such N-rich solids in the interstellar medium, these organic compounds are likely to have formed in the outer regions of the early proto-planetary Solar System (Dartois et al. 2013).

Planetary satellites
Both the atmosphere and the surface of Titan are rich in complex organics. Molecular nitrogen and methane are the primary constituents of the Titan atmosphere. Other organic molecules observed include hydrocarbons, nitriles, and aromatics compounds. The Atacama Large Millimeter/submillimeter Array (ALMA), with its superior spatial resolution, is able to map the distribution of gas-phase molecules such as C 2 H 5 CN, HNC, HC 3 N, CH 3 CN and CH 3 CCH in the Titan atmosphere (Cordiner et al. 2015). The haze in the atmosphere of Titan is believed to be complex hydrocarbon-nitrile compounds. The most popular model of these compounds is tholins. The solar occultation spectra of the Titan atmosphere taken by the Cassini/VIMS instrument show distinct aliphatic signatures in the form of the 3.4 µm feature ). Similar features have also been observed in the atmosphere of Saturn (Kim et al. 2012). Numerous lakes of liquid methane and ethane, probably with other organics dissolved in them, are found on the surface of Titan. Hydrocarbon sand dunes have been estimated to cover ∼20 % of Titan's surface (Lorenz et al. 2008).

Minor planets and outer solar system objects
It is now recognized that the outer Solar System contains a large population of icy objects, which have been referred to as either Kuiper Belt Objects or transneptunian objects (TNOs). The chemical constituents of TNOs are of particular interest because TNOs are believed to be the most primitive bodies in the Solar System. In addition to water ice, ices of N 2 , CH 4 , CO, CO 2 , C 2 H 6 and HCN also exist.
The most prominent member of the TNO family is Pluto. Recent images form the New Horizons spacecraft found that Pluto has a reddish brown color. Since ices are usually colorless, the color of Pluto may be due to complex organics on the surface (Materese et al. 2014). Between the orbits of Jupiter and Neptune minor planets with characteristics between asteroids and comets which are referred to as Centaurs. The colors and reflectance of Centaurs and TNOs have also been used to infer the presence of complex organics in TNOs .

Organics as carriers of unidentified spectral phenomena in the ISM
There are several outstanding mysteries in spectroscopic observations of the interstellar medium which could be traced to organic compounds as their carriers. The origin of diffuse interstellar bands (DIB), 217.5 nm feature, extended red emission (ERE), unidentified infrared emission (UIE) features, and the 21 and 30 µm features have remained unsolved after decades of efforts. Because of the strengths and ubiquitous nature of the features, the carrier must be made up of common and abundant elements, with carbon being the most likely candidate.
It is interesting to note that these phenomena have been observed not only in the diffuse ISM, but also in circumstellar environments, in the galactic halo, and in external galaxies. In some cases they have been observed in galaxies with high redshifts, suggesting that the carriers responsible for these features were already present in the early Universe.

Diffuse interstellar bands
The oldest of these mysteries are the diffuse interstellar bands (DIBs), which have been known for almost a century (Heger 1922). Although more than 500 bands from the near UV to near infrared have been detected, all except two have not been identified (Cami and Cox 2014). In the Milky Way Galaxy, DIBs have been seen towards over one hundred stars. In the Magellanic Clouds, DIBs have been seen in the spectrum of the supernova SN 1987A as well as in the spectra of reddened stars (Ehrenfreund et al. 2002). DIB carriers in the interstellar medium of external galaxies can be probed by supernovae (Sollerman et al. 2005), and DIBs have been detected in external galaxies with redshifts up to 0.5 (Sarre 2006).
DIBs are almost exclusively seen in absorption. The only exception is in the circumstellar envelope of HD 44179 (the Red Rectangle) where several DIB features are seen in emission (Winckel et al. 2002); see also Díaz-Luis et.al (2015) who reported evidence for circumstellar diffuse bands (both in emission and absorption) in the fullerene-containing PN Tc 1.
While the DIBs are widely accepted to be due to electronic transitions of gasphase C-based molecules, the exact chemical structures of the carrier(s) have not been identified. It has been said that DIBs represent the largest reservoir of organic material in the galaxy (Snow 2014). Polycyclic aromatic hydrocarbon (PAH) molecules have been widely discussed as possible candidates of carriers of DIBs (Léger and d'Hendecourt 1985;Salama and Ehrenfreund 2014). However, the electronic transitions of PAH molecules are well known but to date no visible-UV PAH transitions have been detected even after extensive searches (Gredel et al. 2011;Salama et al. 2011).
The most promising case is the identification of two DIBs at 963.2 and 957.7 nm with C + 60 (Foing and Ehrenfreund 1994;Campbell et al. 2015). Two weaker lines of C + 60 at 942.8 and 936.6 nm were also identified with DIBs (Walker et al. 2015). Although the traditional view of the origin of the carriers of DIBs is that they are synthesized and the study of DIBs in C60-rich PNe (García-Hernández and Díaz-Luis 2013) from small gas-phase molecule precursors, the identification of two DIBs with C + 60 suggests the possibility that the DIB carrier molecules may represent breakdown products of large, complex organic compounds, such as mixed aromatic/aliphatic organic nanoparticles (MAON) (Kwok 2014) or other amorphous hydrocarbons (Sect. 7).

The 220 nm feature
The 220 nm extinction feature has been known for about 50 years (Stecher 1965). It was extensively observed by the International Ultraviolet Explorer (IUE) satellite and is found to have a remarkable constancy in its peak wavelength of 217.5 nm, corresponding to an energy gap of 5.7 eV. This is not just a local phenomenon as the feature has been detected in galaxies as distant as redshift >2 (Elíasdóttir et al. 2009).
The carrier of the 220 nm feature is often attributed to a carbonaceous solid such as amorphous carbon (Mennella et al. 1998), carbon onions (Iglesias-Groth 2004), hydrogenated fullerences (Cataldo and Iglesias-Groth 2009), or polycrystalline graphite (Papoular and Papoular 2009). The detection of the 220 nm feature in IDPs with monocrhomated electron energy-loss spectroscopy suggests a possible interstellarsolar system connection (Bradley et al. 2005).

Unidentified infrared emission bands
A family of unidentified infrared emission (UIE) features at 3.3, 6.2, 7.7, 8.6, and 11.3 µm was discovered almost 40 years ago (Russell et al. 1977). The 3.3 µm feature was first identified as the C-H stretching mode of aromatic compounds by Knacke (1977). The organic affiliation was extensively discussed by Duley and Williams (1981), who assigned the 3.3 and 11.3 µm features to graphitic (aromatic) materials. Specifically, the 3.3 µm feature is identified as due to aromatic C-H stretch, the 6.2 µm feature as aromatic C-C stretch, the 8.6 µm feature as the C-H in-plane bending mode, and the 11.3, 12.4 and 13.3 µm features as due to solo, duo and trio C-H out-of-plane bending modes, respectively.
Also present in astronomical spectra are emission features around 3.4 µm, which arise from symmetric and anti-symmetric C-H stretching modes of methyl and methylene groups (Puetter et al. 1979;Geballe et al. 1992). The bending modes of these groups also manifest themselves at 6.9 and 7.3 µm (Jourdain de Muizon et al. 1990;Chiar et al. 2000). In addition, there are unidentified emission features at 15.8, 16.4, 17.4, 17.8, and 18.9 µm, which have been observed in proto-planetary nebulae, reflection nebulae, and galaxies.
The emission bands themselves are often accompanied by strong, broad emission plateaus features at 6-9, 10-15, and 15-20 µm. The first two plateau features have been identified as superpositions of in-plane and out-of-plane bending modes emitted by a mixture of aliphatic side groups attached to aromatic rings (Kwok et al. 2001). The 15-20 µm plateau feature has been detected in young stellar objects, compact Hii regions, and planetary nebulae, but are especially strong in some proto-planetary nebulae (Zhang et al. 2010). A possible origin of this broad feature arises from CCC in-and out-of-plane bending of aromatic rings (Kerckhoven et al. 2000).
The UIE features are always associated with a strong emission continuum which cannot be explained by free-free emission or reflected starlight. For example, scattered starlight is expected to be strongly polarized, but the observed continuum emission is unpolarized. In the diffuse interstellar medium, the strength of the UIE features is strongly correlated with the dust continuum, suggesting that the emission bands are physically related to the continuum (Kahanpää et al. 2003).
The UIE features are seen in very different radiation environments and their emission peak wavelengths and profiles also vary. The energy sources responsible for the excitation of the features have temperatures ranging from tens of thousands of degrees in planetary nebulae (the central star temperature of NGC 7027 is 200,000 K), to ∼30,000 K in Hii regions, and to only thousands of degrees in reflection nebulae and proto-planetary nebulae. The UIE features seen in the reflection nebula NGC 7023 are very similar to those seen in the planetary nebula NGC 7027 in spite of the very different intensities of UV background in the two nebulae.
A variety of chemical structures have been suggested as the carriers of the UIE bands. These include PAH molecules (Léger and Puget 1984;Allamandola et al. 1989),   (Hu and Duley 2008), quenched carbonaceous composite particles (QCC, Sakata et al. 1987), kerogen and coal (Papoular et al. 1989), petroleum fractions (Cataldo et al. 2002), and mixed aromatic/aliphatic organic nanoparticles (MAON, Zhang 2011, 2013). Among these proposed carriers, the PAH hypothesis is by far the most popular. However, the PAH hypothesis has a number of difficulties and its validity has been put into question Sadjadi et al. 2015).
The discovery of fullerene (C 60 ) in the planetary nebula Tc-1 (Cami et al. 2010) has generated interests in possible links between C 60 and the UIE phenomenon. Although Tc-1 has no UIE features, it does show the 8 and 12 µm plateaus (Fig. 3). The protoplanetary nebula IRAS 01005 + 7910, however, show C 60 features, UIE bands, as well as the 8, 12, and 17 µm emission plateau features . The association between C 60 and the 8 and 12 µm plateau features Otsuka et al. 2013) suggests that amorphous carbonaceous solids such as MAONs could be precursors of fullerenes (García-Hernández et al. 2012;Bernard-Salas et al. 2012). PAHs have also been proposed as the C 60 precursors (Berné and Tielens 2012). But the dehydrogenation of PAHs induced by UV photons is more difficult than that of MAONs because the photon energy can quickly spread out within the aromatic nets.

Extended red emission
The observation of the Extended Red Emission (ERE) also goes back 30 years. ERE is commonly seen in reflection nebulae (Witt and Schild 1988;Witt and Boroson 1990), but has also been detected in dark nebulae, cirrus clouds, planetary nebulae, Hii regions, the diffuse interstellar medium, and in haloes of galaxies. The central wavelength of the emission shifts from object to object, or even between locations within the same object. Other than the fact that it may be due to photoluminescence, exact nature of its carrier is still unknown. Other unidentified optical emissions include a set of bright visible bands seen alongside ERE in the Red Rectangle nebula (Schmidt and Witt 1991) and blue luminescence which is seen both in this object and a number of other sources (Vijh et al. 2004).
If the ERE is a result of photoluminescience, the carrier is likely to be a semiconductor with a nonzero band gap and silicon nanoparticles have been suggested as a candidate (Ledoux et al. 1998;Witt et al. 1998). Other possibilities include QCC (Sakata et al. 1992), C 60 (Webster 1993), and nanodiamonds (Chang et al. 2006).

The 21 and 30 µm features
The 21 and 30 µm unidentified infrared features (Fig. 4) are generally associated with objects in the late stages of stellar evolution (Kwok et al. 1989;Forrest et al. 1981), and can be responsible for a significant fraction (up to 8 % for the 21 µm feature and 20 % for the 30 µm feature) of the energy output of the stellar sources (Hrivnak et al. 2000). High resolution ISO observations have found that the 21 µm features have the same intrinsic profile and peak wavelength (20.1 µm) (Volk et al. 1999). There is no evidence for any discrete sub-structure due to molecular bands in the observed spectra, suggesting that the 21-µm feature is either due to a solid substance or a mixture Fig. 4 Combined ISO SWS and LWS and Spitzer IRS spectra of the proto-planetary nebula IRAS 07134+1005 showing the 21 and 30 unidentified emission features. Also seen in the spectra are broad plateau emission features around 8 and 12 µm. All these features sit on top of a strong continuum of many similarly structured large molecules. These features have been detected in evolved stars in the Magellanic Clouds (Volk et al. 2011).
Many proposals for the origin of the 21 µm feature have been made, including hydrogenated fullerenes (Webster 1995), SiC (Speck and Hofmeister 2004), and thiourea groups attached to aromatic/aliphatic structures (Papoular 2011). The first suggestion of the origin of the 30 µm feature is MgS, but it is now considered as unlikely based on abundance grounds (Zhang et al. 2009). Since the 30 µm feature is exclusively seen in carbon-rich objects, an organic carrier is much more plausible. The common correlation between the 21 and 30 µm features with the UIE bands suggests that these phenomena may be related.

Organics in the diffuse ISM
The detection of the 3.4 µm in absorption has led to the realization of the existence of an aliphatic component in the diffuse interstellar medium (Wickramasinghe and Allen 1980). This feature is a superposition of symmetric and anti-symmetric C-H stretching modes arising from methyl (−CH 3 ) and methylene (−CH 2 ) groups in aliphatic hydrocarbons. Since the initial discovery, the 3.4 µm feature has been observed along the line of sight to a number of infrared background sources (Pendleton et al. 1994). High spectral resolution observations are able to resolve the feature into individual CH 2 and CH 3 symmetric and antisymmetric stretching modes (Dartois et al. 2007) (Fig. 5).
Since the derivation of column densities from the strengths of absorption features does not depend on an excitation model, the overall abundance of aliphatic compounds Fig. 5 The 3.4 µm feature is seen in absorption against the background infrared continuum along two lines of sight (GC IRS8 and GCS3) towards the galactic center. Figure adapted from Dartois (2011) can be quite reliably determined. The strength of the 3.4 µm feature suggests that at least 15 % of all the carbon atoms are in the form of aliphatic compounds (Dartois 2011).

Organics in external galaxies
The UIE bands have been detected in planetary nebulae, reflection nebulae, Hii regions, diffuse interstellar medium, and external galaxies. In some active galaxies, up to 20 % of the total luminosity of the galaxy is emitted in the UIE bands (Smith et al. 2007) (Fig. 6). The detection of UIE bands in high-redshift galaxies (Teplitz et al. 2007) and quasars ) implies that complex organics were widely present as early as 10 billion years ago. This suggests that abiological synthesis of complex organics has been occurring through most of the history of the Universe.
A survey of 150 luminous and ultraluminous galaxies by the AKARI satellite has resulted in common detection of the 3.3 µm emission feature. The observed fraction of total energy emitted in the 3.3 µm band is ∼10 −3 (Imanishi et al. 2010).
In addition, the 3.4 and 6.9 µm aliphatic C-H stretching and bending modes have been detected in absorption in our own and other galaxies. Strong 3.4 µm absorption features can be seen in absorption in ultraluminous infrared galaxies (Mason et al. 2004;Imanishi et al. 2010). Figure 7 shows the 3.4 µm feature in absorption next to the 3.3 µm emission feature (Risaliti et al. 2006).
Since the UIE bands are commonly used to trace star formation and to probe the radiation field of galaxies assuming that PAH molecules are the carrier (Valiante et al.   Risaliti et al. (2006) 2007; Pope et al. 2013), a correct identification of the UIE bands are essential for our understanding of the galactic environment.

Laboratory simulations of interstellar organics
In order to identify possible carriers of the unidentified spectral phenomena discussed in Sect. 4, it would be useful to see what carbonaceous products can naturally exist in the interstellar medium. By introducing H into graphite (sp 2 ) and diamond (sp 3 ), a variety of amorphous C-H alloys can be created (Cataldo 2004;Jones 2012a, b, c;Jones et al. 2013). Different geometric structures with long-and short-range can be created by varying the aromatic to aliphatic ratios. A schematic of possible structures of amorphous carbonaceous solids is shown in Fig. 8. The lower left corner of the triangle represents graphite, the top corner represents diamonds, PAHs are on the bottom edge, and various forms of amorphous hydrogenated carbon can exist in the interior of the triangle. The infrared spectra of these amorphous carbonaceous materials (Dischler et al. 1983) resemble the astronomical UIE bands seen in planetary nebulae and proto-planetary nebulae (Fig. 9). Since these amorphous carbonaceous solids have absorption bands in the visible, they can be easily excited by visible light from stars.
Organic particles of such structures are natural products of combustion. The first nucleation products for soot particles formed in flames have structures consisting of islands of aromatic rings linked by chains. Identified sidegroups in soot include methyl (−CH 3 ), methylene (−CH 2 ), carbonyl (C=O), aldehydic (−HCO), phenolic (−OH),  (Pino et al. 2008). Similar combustion processes may be at work in carbon-rich circumstellar envelopes.
By the early 1980s, it was known that carbon clusters can be produced by laser vaporization of graphite followed by supersonic expansion into an inert gas. The employment of this technique has led to the discovery of fullerene, a new form of carbon (Kroto et al. 1985). Since then, various techniques based on laser pyrolysis of gas-phase hydrocarbons followed by condensation have been used to create laboratory counterparts of cosmic organic dust (Jäger et al. 2009). These include the quenching of plasma of 4-torr methane (Sakata et al. 1987), hydrocarbon flame or arc-discharge in a neutral of hydrogenated atmosphere (Colangeli et al. 2003;Mennella et al. 2003), laser ablation of graphite in a hydrogen atmosphere (Scott and Duley 1996;Mennella et al. 1999), infrared laser pyrolysis of gas phase molecules (C 2 H 4 , C 4 H 6 ) (Herlin et al. 1998), photolysis of methane at low temperatures (Dartois et al. 2004), and flame combustion of C 2 H 2 , C 2 H 4 , C 3 H 6 mixed with O 2 , forming soot (Pino et al. 2008).
In addition to soot, there are also other natural products such as coal and kerogen that have similar amorphous mixed aromatic/aliphatic properties (Guillois et al. 1996;Papoular 2001). The infrared spectra of petroleum and asphaltenes also show spectral features similar to astronomical UIE bands (Cataldo et al. 2002(Cataldo et al. , 2013.

Origin and distribution of complex organics in the Universe
Complex organics are now known to be widely present in the Universe, from Solar System objects to distant galaxies. These organics are synthesized abiologically, and do not represent breakdown products of living organisms. In contrast, almost all of the complex organics on Earth are biological in origin, making the Earth an exception to the wide presence of abiological organics in the Universe.
Although the exact pathways of synthesis are not known, it is widely believed that these complex organics are synthesized from simple organic molecules, either through gas-phase reactions or chemical reactions on solid-state surfaces. In the astronomical community, there is a lot of interest on the possibility of organic synthesis taking place in star forming regions, as there are heavy concentrations of gas-phase organics in these objects. In the space science community, the origin of complex organics in Solar System objects is often traced to the early epochs of the Solar System, although transport from interstellar medium to the primordial solar nebula has also been discussed.
The only concrete observational evidence for organic synthesis exists in circumstellar envelopes. During the asymptotic-giant-branch phase of evolution, the element carbon is produced by triple-α reactions in the stellar core and brought to the surface via convection. Due to the extended atmosphere and low surface temperatures of these stars, simple molecules such as C 2 , C 3 , and CN are formed in the stellar atmosphere and ejected by a stellar wind. In the circumstellar envelopes formed by stellar wind outflows, over 80 gas-phase molecules, including organics (C 2 H 2 , CH 4 , H 2 CO, CH 3 CN), radicals (C 2 H, C 3 , HCO + ), rings (C 3 H 2 ), and chains (HC 3 N, HC 5 N, HC 7 N), are synthesized. All these molecules are formed within the dynamical timescales of the outflow, which is ∼10 4 years. After the stellar wind completely deplete the stellar envelope, and circumstellar environment is exposed to increasingly more energetic radiation field as the stellar core is gradually exposed. It is at this stage that aromatic and aliphatic compounds, as well as fullerenes are formed. We therefore have extremely strong observational constraints that complex organics are formed in a low-density environment over very short (10 3 years) time scales (Kwok 2004).
Since over 90 % of all stars in the Galaxy go through this stage of evolution, a very large amount of complex organics are created by stars. We also know that these organic products are distributed to the interstellar medium through stellar winds. Whether these organic materials are destroyed or further processed in the interstellar medium, we do not know. It would not be unreasonable to assume that the early Solar System inherited some of these stellar material, as the IOM of meteorites show remarkable similarities to stellar produced organics.
Since the organic signatures are particularly strong in ultraluminous galaxies, it is natural to assume that the synthesis and/or excitation of organics in galaxies are related to the star formation process. Since the spectra of galaxies represent integrated light output from the entire galaxy, we do not have any information on the spatial distribution or origin of such organics. We do know, however, that organic synthesis happened in the Universe almost as soon as carbon is synthesized, and organic synthesis is common in the Universe.
The inner Solar System, including the early Earth, was extensively bombarded by external objects between 4.5 to 3.8 billion years ago. This has led to speculations on externally delivered organics to Earth may have influenced the origin of life on Earth (Anders 1989;Chyba and Sagan 1992). It is estimated that the amount of extraterrestrial organics delivered to Earth by comets, asteroids, and IDPs during the heavy bombardment period exceed those created from terrestrial sources through UV photolysis, electric discharge or from hydrothermal vents by several orders of magnitude (Ehrenfreund et al. 2002). To what extent that these extraterrestrial organics can survive intact during delivery is dependent on the mechanism of energy loss during the passage through the atmosphere. Energy loss through radiation or ablation has to exceed that of thermal decomposition of organics in order for the organics to remain intact upon impact. It is expected that smaller particles such as IDP may be more efficient in the delivery of organics (Pasek 2016).
If external delivery of organics played a major role in the development of life on Earth, then similar circumstances will also apply to other planetary systems in the Galaxy. Since planetary systems are now known to be common in our Galaxy (Winn and Fabrycky 2015), similar organic enrichment by stellar ejecta may have occurred in other planetary systems.

Outlook
Although the wide presence of extraterrestrial complex organics was not expected just a couple decades ago, observational evidence has completely changed our preconceived theoretical notions. With new large millimeter-wave arrays such as ALMA, more and more complex gas-phase organics will likely be detected, including possibly simple amino acids and building blocks of carbohydrates, lipids and nucleic acids. For a better determination of the chemical structure of organics in stars, interstellar clouds and galaxies, we need infrared space missions capable of high spectroscopic resolution observations. Space missions to Mars, planetary satellites, comets and asteroids have the potential of direct detection of complex organics in an ever widening types of environments. All these observations and measurements need to be accompanied by extensive laboratory analysis and simulations for correct identification of the chemical species. The study of complex organics in space has significant implications on the origin of life on Earth as well as our perception of our place in the Universe.