1. Ross, D. A. and HUNT, J. M., 1967, Third Brine Pool in the Red Sea: Nature: v. 213, no. 5077: p. 687-688.

BibTeX
@article{ross1967third,
    author = "Ross, D. A. and HUNT, J. M.",
    title = "Third Brine Pool in the Red Sea",
    year = "1967",
    journal = "Nature",
    url = "https://doi.org/10.1038/213687a0",
    doi = "10.1038/213687a0",
    number = "5077",
    pages = "687-688",
    volume = "213"
}

2. Ku, Teh-Lung, 1969, Uranium Series Isotopes in Sediments from the Red Sea Hot-Brine Area: Hot Brines and Recent Heavy Metal Deposits in the Red Sea: p. 512-524.

BibTeX
@incollection{ku1969uranium,
    author = "Ku, Teh-Lung",
    title = "Uranium Series Isotopes in Sediments from the Red Sea Hot-Brine Area",
    year = "1969",
    booktitle = "Hot Brines and Recent Heavy Metal Deposits in the Red Sea",
    url = "https://doi.org/10.1007/978-3-662-28603-6\_45",
    doi = "10.1007/978-3-662-28603-6\_45",
    pages = "512-524"
}

3. Ostapoff, Feodor, 1969, A Fourth Brine Hole in the Red Sea?: Hot Brines and Recent Heavy Metal Deposits in the Red Sea: p. 18-21.

BibTeX
@incollection{ostapoff1969a,
    author = "Ostapoff, Feodor",
    title = "A Fourth Brine Hole in the Red Sea?",
    year = "1969",
    booktitle = "Hot Brines and Recent Heavy Metal Deposits in the Red Sea",
    url = "https://doi.org/10.1007/978-3-662-28603-6\_4",
    doi = "10.1007/978-3-662-28603-6\_4",
    pages = "18-21"
}

4. 1972, More Red Sea Brine Pools: Nature: v. 240, no. 5381: p. 384-384.

BibTeX
@article{crossref1972more,
    title = "More Red Sea Brine Pools",
    year = "1972",
    journal = "Nature",
    url = "https://doi.org/10.1038/240384b0",
    doi = "10.1038/240384b0",
    number = "5381",
    pages = "384-384",
    volume = "240"
}

5. Ross, D A, 1972, Red sea hot brine area: revisited.: Science (New York, N.Y.).

Abstract

A return expedition to the hot brine area of the Red Sea in 1971 found that the temperature of the brine had increased, indicating that the process that formed the underlying deposits rich in heavy metals is still occurring. About 0.346 cubic kilometers of water having a minimum temperature of 104 degrees C has been added over the last 52 months. Calculations suggest that this water may have come from a relatively shallow depth; this result coupled with the fact that fracture zones are found north and south of the brine area indicates a relatively local source for the brine, rather than the Strait of Bab el Mandeb, as previously suggested.

BibTeX
@article{doi101126science17540291455,
    author = "Ross, D A",
    title = "Red sea hot brine area: revisited.",
    year = "1972",
    journal = "Science (New York, N.Y.)",
    abstract = "A return expedition to the hot brine area of the Red Sea in 1971 found that the temperature of the brine had increased, indicating that the process that formed the underlying deposits rich in heavy metals is still occurring. About 0.346 cubic kilometers of water having a minimum temperature of 104 degrees C has been added over the last 52 months. Calculations suggest that this water may have come from a relatively shallow depth; this result coupled with the fact that fracture zones are found north and south of the brine area indicates a relatively local source for the brine, rather than the Strait of Bab el Mandeb, as previously suggested.",
    url = "https://pubmed.ncbi.nlm.nih.gov/17842283/",
    doi = "10.1126/science.175.4029.1455",
    pmid = "17842283"
}

6. Ross, David A., 1972, Red Sea Hot Brine Area: Revisited: Science: v. 175, no. 4029: p. 1455-1457.

Abstract

A return expedition to the hot brine area of the Red Sea in 1971 found that the temperature of the brine had increased, indicating that the process that formed the underlying deposits rich in heavy metals is still occurring. About 0.346 cubic kilometers of water having a minimum temperature of 104°C has been added over the last 52 months. Calculations suggest that this water may have come from a relatively shallow depth; this result coupled with the fact that fracture zones are found north and south of the brine area indicates a relatively local source for the brine, rather than the Strait of Bab el Mandeb, as previously suggested.

BibTeX
@article{ross1972red,
    author = "Ross, David A.",
    title = "Red Sea Hot Brine Area: Revisited",
    year = "1972",
    journal = "Science",
    abstract = "A return expedition to the hot brine area of the Red Sea in 1971 found that the temperature of the brine had increased, indicating that the process that formed the underlying deposits rich in heavy metals is still occurring. About 0.346 cubic kilometers of water having a minimum temperature of 104°C has been added over the last 52 months. Calculations suggest that this water may have come from a relatively shallow depth; this result coupled with the fact that fracture zones are found north and south of the brine area indicates a relatively local source for the brine, rather than the Strait of Bab el Mandeb, as previously suggested.",
    url = "https://doi.org/10.1126/science.175.4029.1455",
    doi = "10.1126/science.175.4029.1455",
    number = "4029",
    pages = "1455-1457",
    volume = "175"
}

7. Ross, D. A, 1972, Red Sea hot brine area revisited.

BibTeX
@misc{ross1972red1,
    author = "Ross, D. A",
    title = "Red Sea hot brine area revisited",
    year = "1972",
    howpublished = "Science, v. 175, p. 1455- 1457",
    note = "talkorigins\_source = {true}; raw\_reference = {Ross, D. A., 1972, Red Sea hot brine area revisited: Science, v. 175, p. 1455- 1457.}"
}

8. 1973, Differences between Red Sea Brine Pools: Nature: v. 241, no. 5391: p. 503-503.

BibTeX
@article{crossref1973differences,
    title = "Differences between Red Sea Brine Pools",
    year = "1973",
    journal = "Nature",
    url = "https://doi.org/10.1038/241503c0",
    doi = "10.1038/241503c0",
    number = "5391",
    pages = "503-503",
    volume = "241"
}

9. DOWLER, M. J. and INGMANSON, D. E., 1979, Thiocyanate in Red Sea brine and its implications: Nature: v. 279, no. 5708: p. 51-52.

BibTeX
@article{dowler1979thiocyanate,
    author = "DOWLER, M. J. and INGMANSON, D. E.",
    title = "Thiocyanate in Red Sea brine and its implications",
    year = "1979",
    journal = "Nature",
    url = "https://doi.org/10.1038/279051a0",
    doi = "10.1038/279051a0",
    number = "5708",
    pages = "51-52",
    volume = "279"
}

10. Ingmanson, D. E. and Dowler, M. J., 1980, Unique amino acid composition of Red Sea brine: Nature: v. 286, no. 5768: p. 51-52.

BibTeX
@article{ingmanson1980unique,
    author = "Ingmanson, D. E. and Dowler, M. J.",
    title = "Unique amino acid composition of Red Sea brine",
    year = "1980",
    journal = "Nature",
    url = "https://doi.org/10.1038/286051a0",
    doi = "10.1038/286051a0",
    number = "5768",
    pages = "51-52",
    volume = "286"
}

11. Kaartvedt, Stein and Antunes, André and Røstad, Anders and Klevjer, Thor A. and Vestheim, Hege, 2016, Zooplankton at deep Red Sea brine pools: Journal of Plankton Research: v. 38, no. 3: p. 679-684.

BibTeX
@article{kaartvedt2016zooplankton,
    author = "Kaartvedt, Stein and Antunes, André and Røstad, Anders and Klevjer, Thor A. and Vestheim, Hege",
    title = "Zooplankton at deep Red Sea brine pools",
    year = "2016",
    journal = "Journal of Plankton Research",
    url = "https://doi.org/10.1093/plankt/fbw013",
    doi = "10.1093/plankt/fbw013",
    number = "3",
    pages = "679-684",
    volume = "38"
}