3.7 billion year old biogenic remains.

3.7 Billion year old inclusions inside garnet crystals contain 13C depleted carbonaceous material consistent with biogenic origin. Additional evidence in the form of the other elements of life mainly O, N and P were found to be structural bound to this material by using a new technique, AFM-IR. Here we show additional evidence that support our claim. By overlaying maps generated by the AFM-IR we show how the location of 100's of nm sized contiguous domains of nitrile and possibly phosphonate overlap inside the inclusion. This shows that O, N and P are not only co-localized to the same inclusion but they are co-localized to the same patch of carbonaceous material inside the inclusion. They therefore provide spatial characterization for potentially the oldest biogenic remains in Earth's geological record and corroborates earlier claims2 for the biogenic origins of carbon in Isua metasediments.

3.7 billion years old metasedimentary rocks from Isua, West Greenland contain trails of n class="Chemical">carbonaceousn> compounds, with isotopn>ic ratios consistent with biogenic origin. The n>an class="Chemical">carbonaceous material form trails of contiguous inclusions across Metamorphic garnet crystals inside the host rock. We have recently shown how the other elements of life (mainly oxygen, nitrogen and possibly phosphor) is structurally bound to this carbonaceous material that has been trapped inside these inclusions since their formation 3.7 billion years ago. By in situ infrared absorption with a spatial resolution in nanometer regime within these inclusions we have generated spectra and maps showing the distribution of nitrile and the presence of oxygen in form of anhydride and carboxyl groups and possibly phosphor in the form of phosphonate. These results were found to be consistent with µm^3 remains of biogenic material isolated for billions of years.

The instrument used for generating the maps and spectra shown here and in the original manuscript was an atomic force microscopy (AFM) equipped with a tuneable IR (infrared) laser (AFM-IR) that is able to record IR absorption information with nanometer resolution on surfaces suitable for AFM.

Figure 1 shows part of an inclusion found inside a garnet crystal (Fig. 1a). The internal surface inside the inclusion was covered with 100–500 nm thick n class="Chemical">pan class="Chemical">carbonaceous material. In Fig. 1b we have dispn>layed an IR absorption map consistent with n>an class="Chemical">nitrile (2230 cm−1) (green most intense) combined with IR absorption consistent with phosphonate (960 cm−1/1270 cm−1) (red/pink most intense). The primary absorptions for phosphonate at 1040 cm−1 and 1160 cm−1 was for technical reasons too intense for making maps.

Figure 1.

Nitrogen and phosphonate bound to the carbonaceous material inside a 3.7 billion old inclusion. a) AFM deflection image. Everything to the left of the black line shows the internal surface of the inclusion and it is covered with carbonaceous material, while to the right of the black line, the surface is a clean garnet surface. b) Map of absorption consistent with nitrile (Green (2230 cm−1)) combined with a map of absorption consistent with phosphonate (red (940 cm−1) pink (1280 cm−1)) dark blue represent zero absorption at these three wavelengths. c) Two representative absorption spectra at locations indicated in b) (the absorption intensity is shown with a logarithmic scale).

pan class="Chemical">Nitrogenn> and pan class="Chemical">phosphonate bound to the pan class="Chemical">carbonaceous material inside a 3.7 billion old inclusion. a) AFM deflection image. Everything to the left of the black line shows the internal surface of the inclusion and it is covered with carbonaceous material, while to the right of the black line, the surface is a clean garnet surface. b) Map of absorption consistent with nitrile (Green (2230 cm−1)) combined with a map of absorption consistent with phosphonate (red (940 cm−1) pink (1280 cm−1)) dark blue represent zero absorption at these three wavelengths. c) Two representative absorption spectra at locations indicated in b) (the absorption intensity is shown with a logarithmic scale).

The maps suggest that the distribution of the two comn class="Chemical">pounds was heterogeneous inside the inclusion since for most regions of the carbonaceous material inside the inclusion there was either none or only traces of either n>an class="Chemical">nitrile or phosphonate. But in some patches, there was a high IR absorption in distinct domains ranging from 100 nm to 1 µm across. These high absorption domains for the two compounds roughly overlapped, so on the map there was roughly three distinct patches approximately 1 µm across where the density of the compounds was increased compared to the background level.

Also, shown in the figure (Fig. 1c) are two spectra recorded where the two tyn class="Chemical">pes of compounds were co-located. In the plot, we have shown the intensity on a logarithmic scale since the absorption consistent with phosphonate was very intense. The position of the absorption peaks in the spn>ectra consistent with pn>an class="Chemical">phosphonate bonded to aromatic molecules is around 960, 1040, 1160, 1270 cm−1[6] most of which are present in both spectra. In spectra S1 there is also an absorption at 1660 which could be caused by C=C bonds. In these two spectra, there was no evidence for anhydride or carboxyl groups at 1824 cm−1 and 1720 cm−1 respectively, so the oxygen was only found with the phosphonate. Finally, the absorption for nitrile can be found at 2230 cm−1

In the original pan class="Chemical">per, we concluded that the structural binding of nitrogen, n>an class="Chemical">oxygen and phosphorous to the carbonaceous material inside the inclusions was evidence for biogenic origin of the carbonaceous material. The map shown in Fig. 1 not only demonstrate that nitrogen, oxygen and phosphor were structurally bound to the carbonaceous material inside the inclusion but the compounds were in this case co-located in patches approximately 1µm across. This co-localization of the compounds was not just in the same inclusion but in the same patch of carbonaceous material inside the inclusion which therefore lends further support to the biogenic origin of this material.