Archive image from page 17 of The Danish Ingolf-expedition (1899-1953). The Danish Ingolf-expedition danishingolfex4cpt11daniuoft Year: 1899-1953 TOMOFTERIDjE AND typhloscolecid. always found near the surface of the ocean, entered these two areas, viz: the Irminger Sea and the Davis Strait? They have probably followed the branch of the North Atlantic Drift which W. of Ireland turns north- wards and, following the south and west coast of Iceland, enters the northern part of the Denmark Strait. Part of this current transforms into the cold East Greenland current, which turns round Cape Farewel
Archive image from page 17 of The Danish Ingolf-expedition (1899-1953). The Danish Ingolf-expedition danishingolfex4cpt11daniuoft Year: 1899-1953 TOMOFTERIDjE AND typhloscolecid. always found near the surface of the ocean, entered these two areas, viz: the Irminger Sea and the Davis Strait? They have probably followed the branch of the North Atlantic Drift which W. of Ireland turns north- wards and, following the south and west coast of Iceland, enters the northern part of the Denmark Strait. Part of this current transforms into the cold East Greenland current, which turns round Cape Farewell, and running ters the Davis Strait. In the summer season the surface water in this strait Q 7 helgolandica (» T. Nissi m X T. KefersU ini - T ' at >ill11 Textfigure i attains such high temperatures that a priori we are allowed to suppose that T. Nisseni may thrive here. (Both hauls in the Davis Strait were made in the height of the summer). This accounts for the occurrence of the ies 11 south of the submarine ridge across the Davis Strait between Holstensborg and Cape Wolsingham in Baffin Land and 2) W. of Iceland, and, finally, 3) for the non-occurrence of the species at the coast of East i Greenland. There is only little probability that it will extend beyond the above mentioned ridge or be found in the sen north and easl oi [< eland (The Norwegian Sea), as the temperature of the water in these localities will be too low for the species to subsist there. We are allowed to presume that larger materials of pelagic
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