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   <subfield code="a">Mountain-block recharge, present and past, in the eastern Española Basin, New Mexico, USA</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Andrew Manning]</subfield>
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   <subfield code="a">Recharge actuelle et passée d'un massif montagneux, partie orientale du bassin Española, New Mexico, USA</subfield>
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   <subfield code="a">Recarga en un bloque montañoso, presente y pasado en la Cuenca Española oriental, New Mexico, EEUU</subfield>
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   <subfield code="a">Recarga actual e histórica em blocos montanhosos da Bacia Espanhola oriental, Novo México, EUA</subfield>
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   <subfield code="a">Noble gas recharge temperatures (NGTs) and radiocarbon ages were determined for 43 groundwater samples collected in the eastern Española Basin, New Mexico (USA), to identify mountain-block recharge in waters &lt;10 thousand years (ka) old and to evaluate possible changes in mountain-block recharge over the past ∼35ka. For Holocene samples from the southeastern area, NGTs are dominantly 2-4° cooler than the measured water-table temperature near the mountain front. Computed minimum mountain-block recharge fractions are dominantly 0.2-0.5, consistent with previous large mountain-block recharge estimates. NGTs do not display the distinct low during the last glacial maximum observed in other paleorecharge studies; samples recharged 15-25ka ago are on average only 1.3° cooler than Holocene samples. Instead, samples with the coldest NGTs were recharged 25-35ka ago. A proposed explanation is that higher precipitation rates during the last glacial maximum resulted in a lower mean recharge elevation for the basin, essentially buffering the effect of the lower mean annual air temperature and producing NGTs similar to the Holocene. In the period preceding the last glacial maximum, precipitation rates more like today's resulted in Holocene-like mountain-block recharge fractions, producing a mean NGT ∼5° cooler than the Holocene, as expected.</subfield>
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