![]() | |
![]() | |
Names | |
---|---|
Preferred IUPAC name [(2R,7R,11R,15S,19S,22S,26S,30R,34R,38R,43R,47R,51S,55S,58S,62S,66R,70R)-7,11,15,19,22,26,30,34,43,47,51,55,58,62,66,70-Hexadecamethyl-1,4,37,40-tetraoxacyclodoheptacontane-2,38-diyl]dimethanol | |
Other names
| |
Identifiers | |
3D model (JSmol) | |
ChemSpider | |
PubChem CID | |
| |
| |
Properties | |
C86H172O6 | |
Molar mass | 1302.28 g/mol |
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa). |
Caldarchaeol is a membrane-spanning lipid of the isoprenoid glycerol dialkyl glycerol tetraether (iGDGT) class, produced and used by archaea. [1] Membranes made up of caldarchaeol are more stable since the hydrophobic chains are linked together (as compared to lipid bilayer structures in eukaryotes and bacteria), allowing archaea to withstand extreme conditions.
Caldarchaeol is also known as dibiphytanyl diglycerol tetraether, or GDGT-0. Two glycerol units are linked together by two biphytanes, each of which consist of two phytanes linked together to form a linear chain of 32 carbon atoms (40 carbons including methyl branches).
The configuration of the macrocyclic tetraether has been determined by total synthesis of the C40-diol and comparison with a sample obtained by degradation of natural tetraether. [2] A synthesis of tetraether has also been carried out. [3]
Caldarchaeol is not currently described as having any hazards. Due to its high molecular weight, it is neither volatile nor flammable. Caldarchaeol and other GDGTs are present across environments at low concentrations, and no adverse affects or evidence of toxicity are known.
Nomenclature for archaeal lipids is widely varied across history and fields, and caldarchaeol is no exception. It had originally been defined as dibiphytanyl diglycerol tetraether, [4] [5] a large lipid molecule with two biphytane chains, with or without cyclopentane rings, connected by ethers to glycerols on either end. It is used to describe the entire class of isoprenoid GDGTs in many papers, both historical and recent. [5] [6] [7] [8] However, as GDGTs began to be incorporated into paleoclimate investigations, many began defining caldarchaeol specifically as GDGT-0, the isoprenoid GDGT with no cyclopentane moieties, especially when this specific structure is used in the analysis. [9] [10] [11] [12] [13]
Caldarchaeol is the most widely spread GDGT in the archaea domain, found in every major archaeal clade except halophiles. [7] Caldarchaeol, as well as other GDGTs, were previously thought to be specific to hot environments, partially due to the assumption that archaea are only found at these temperatures [14] . However, as archaea continue to be isolated from more environmental types, the discovery of caldarchaeol across temperature, chemical, and physical conditions continues as well [5] [12] [15] [16] [17] [18] [19] [20] .
The biosynthesis of caldarchaeol and other iGDGTs has been the subject of investigation for decades, due both to the complexity of the pathway and the difficulty of culturing archaea in laboratory settings. Isoprenoid-based molecules are synthesized by all three domains of life using isopentyl pyrophosphate (IPP) and dimethylallyl pyrophosphate (DMAPP), 5-carbon structural isomers. Archaea make archaeol from these building blocks [22] , which is then condensed into tetraether structures using a radical S-adenosylmethionine (SAM) protein called tetraether synthase (Tes) [21] .
Caldarchaeol is a widely distributed lipid across archaea, making it a relatively poor biomarker for specific taxa within the domain. However, comparisons between caldarchaeol concentrations and other biomarkers are frequently used to reveal community composition and/or paleoclimate proxies.
Formula: Caldarchaeol/Crenarchaeol
Formula: TEX₈₆ = ([GDGT-2] + [GDGT-3] + [Cren']) / ([GDGT-1] + [GDGT-2] + [GDGT-3] + [Cren'])
Formula: ACE = 100 × ([archaeol] / ([archaeol] + [caldarchaeol]))