Mackenzie E. Gerringer
University of Hawaii
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Featured researches published by Mackenzie E. Gerringer.
Proceedings of the National Academy of Sciences of the United States of America | 2014
Paul H. Yancey; Mackenzie E. Gerringer; Jeffrey C. Drazen; Ashley A. Rowden; Alan J. Jamieson
Significance Fish appear to be absent from the oceans greatest depths, the trenches from 8,400–11,000 m. The reason is unknown, but hydrostatic pressure is suspected. We propose that the answer is the need for high levels of trimethylamine oxide (TMAO, common in many marine animals), a potent stabilizer capable of counteracting the destabilization of proteins by pressure. TMAO is known to increase with depth in bony fishes (teleosts) down to 4,900 m. By capturing the worlds second-deepest known fish, the hadal snailfish Notoliparis kermadecensis from 7,000 m, we find that they have the highest recorded TMAO contents, which, moreover, yield an extrapolated maximum for fish at about 8,200 m. This is previously unidentified evidence that biochemistry may constrain depth for a large taxonomic group. No fish have been found in the deepest 25% of the ocean (8,400–11,000 m). This apparent absence has been attributed to hydrostatic pressure, although direct evidence is wanting because of the lack of deepest-living species to study. The common osmolyte trimethylamine N-oxide (TMAO) stabilizes proteins against pressure and increases with depth, going from 40 to 261 mmol/kg in teleost fishes from 0 to 4,850 m. TMAO accumulation with depth results in increasing internal osmolality (typically 350 mOsmol/kg in shallow species compared with seawaters 1,100 mOsmol/kg). Preliminary extrapolation of osmolalities of predicted isosmotic state at 8,000–8,500 m may indicate a possible physiological limit, as greater depths would require reversal of osmotic gradients and, thus, osmoregulatory systems. We tested this prediction by capturing five of the second-deepest known fish, the hadal snailfish (Notoliparis kermadecensis; Liparidae), from 7,000 m in the Kermadec Trench. We found their muscles to have a TMAO content of 386 ± 18 mmol/kg and osmolality of 991 ± 22 mOsmol/kg. These data fit previous extrapolations and, combined with new osmolalities from bathyal and abyssal fishes, predict isosmotic state at 8,200 m. This is previously unidentified evidence that biochemistry could constrain the depth of a large, complex taxonomic group.
Zootaxa | 2017
Mackenzie E. Gerringer; Thomas D. Linley; Alan J. Jamieson; Erica Goetze; Jeffrey C. Drazen
Pseudoliparis swirei sp. nov. is described from 37 individuals collected in the Mariana Trench at depths 6898-7966 m. The collection of this new species is the deepest benthic capture of a vertebrate with corroborated depth data. Here, we describe P. swirei sp. nov. and discuss aspects of its morphology, biology, distribution, and phylogenetic relationships to other hadal liparids based on analysis of three mitochondrial genes. Pseudoliparis swirei sp. nov. is almost certainly endemic to the Mariana Trench, as other hadal liparids appear isolated to a single trench/ trench system in the Kermadec, Macquarie, South Sandwich, South Orkney, Peru-Chile, Kurile-Kamchatka and Japan trenches. The discovery of another hadal liparid species, apparently abundant at depths where other fish species are few and only found in low numbers, provides further evidence for the dominance of this family among the hadal fish fauna.
Royal Society Open Science | 2017
Mackenzie E. Gerringer; Jeffrey C. Drazen; Thomas D. Linley; Adam P. Summers; Alan J. Jamieson; Paul H. Yancey
Many deep-sea fishes have a gelatinous layer, or subdermal extracellular matrix, below the skin or around the spine. We document the distribution of gelatinous tissues across fish families (approx. 200 species in ten orders), then review and investigate their composition and function. Gelatinous tissues from nine species were analysed for water content (96.53 ± 1.78% s.d.), ionic composition, osmolality, protein (0.39 ± 0.23%), lipid (0.69 ± 0.56%) and carbohydrate (0.61 ± 0.28%). Results suggest that gelatinous tissues are mostly extracellular fluid, which may allow animals to grow inexpensively. Further, almost all gelatinous tissues floated in cold seawater, thus their lower density than seawater may contribute to buoyancy in some species. We also propose a new hypothesis: gelatinous tissues, which are inexpensive to grow, may sometimes be a method to increase swimming efficiency by fairing the transition from trunk to tail. Such a layer is particularly prominent in hadal snailfishes (Liparidae); therefore, a robotic snailfish model was designed and constructed to analyse the influence of gelatinous tissues on locomotory performance. The model swam faster with a watery layer, representing gelatinous tissue, around the tail than without. Results suggest that the tissues may, in addition to providing buoyancy and low-cost growth, aid deep-sea fish locomotion.
Deep Sea Research Part I: Oceanographic Research Papers | 2016
Thomas D. Linley; Mackenzie E. Gerringer; Paul H. Yancey; Jeffrey C. Drazen; Chloe L. Weinstock; Alan J. Jamieson
Deep Sea Research Part I: Oceanographic Research Papers | 2017
Thomas D. Linley; A.L. Stewart; P.J. McMillan; Malcolm R. Clark; Mackenzie E. Gerringer; Jeffrey C. Drazen; Toyonobu Fujii; Alan J. Jamieson
Deep Sea Research Part I: Oceanographic Research Papers | 2015
Jeffrey C. Drazen; Jason R. Friedman; Nicole E. Condon; Erica J. Aus; Mackenzie E. Gerringer; Aimee A. Keller; M. Elizabeth Clarke
Deep Sea Research Part I: Oceanographic Research Papers | 2017
Mackenzie E. Gerringer; Jeffrey C. Drazen; Paul H. Yancey
Deep Sea Research Part I: Oceanographic Research Papers | 2017
Mackenzie E. Gerringer; Brian N. Popp; Thomas D. Linley; Alan J. Jamieson; Jeffrey C. Drazen
Archive | 2017
Mackenzie E. Gerringer; Jeffrey C. Drazen; Thomas D. Linley; Adam P. Summers; Alan J. Jamieson; Paul H. Yancey
Deep-Sea Research Part I: Oceanographic Research Papers | 2017
Mackenzie E. Gerringer; A.H. Andrews; G.R. Huss; K. Nagashima; Brian N. Popp; Thomas D. Linley; N.D. Gallo; Malcolm R. Clark; Alan J. Jamieson; Jeffrey C. Drazen